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  • 1
    Call number: S 91.0718(164/165) / Regal 44/3+4
    In: Procès-verbaux des ... séances de la Commission Géodésique Suisse
    Type of Medium: Series available for loan
    Pages: 20 S.
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  • 2
    Call number: S 91.0718(162/163) / Regal 44/3+4
    In: Procès-verbaux des ... séances de la Commission Géodésique Suisse
    Type of Medium: Series available for loan
    Pages: 22 S.
    Location: Magazine - must be ordered
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  • 3
    Series available for loan
    Series available for loan
    Sevres
    Associated volumes
    Call number: S 98.0553(3) / Mag. 38
    In: Rapport du directeur sur l'activité et la gestion du Bureau international des Poids et Mesures (BIPM)
    Type of Medium: Series available for loan
    Pages: 237 S.
    ISBN: 9282221946
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  • 4
    Monograph available for loan
    Monograph available for loan
    Sverdlovsk : Akad. Nauk SSSR, Uralskij Filial
    Call number: G 682/39 / C3
    Type of Medium: Monograph available for loan
    Pages: 494 S.
    Series Statement: Trudy Gorno-Geologičeskogo Instituta / Akademija Nauk SSSR, Uralskij Filial 39
    Location: Magazine - must be ordered
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  • 5
    Call number: AWI E2-91-1522 ; M 03.0403 / Regal 13
    Type of Medium: Monograph available for loan
    Pages: 303 S. + Portr.
    Edition: 5. Aufl.
    Location: Magazine - must be ordered
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  • 6
    Series available for loan
    Series available for loan
    Berlin : Nationalkomitee für Geodäsie und Geophysik bei der Akademie der Wissenschaften der DDR
    Associated volumes
    Call number: MOP Per 581 ; MOP Per 581(1/11) ; ZSP-319/A-11
    In: Geodätische und geophysikalische Veröffentlichungen : Reihe 1, Heft 11
    Type of Medium: Series available for loan
    Pages: 63 Seiten , Illustrationen
    ISSN: 0533-7577
    Series Statement: Geodätische und geophysikalische Veröffentlichungen : Reihe 1 11
    Language: German
    Note: Inhalt: I. Untersuchungen zur Avifauna von King George / R. Bannasch und U. Lundberg. - II. Robbenbeobachtungen im Gebiet von King George / R. Bannasch. - III. Beobachtungen der marinen Fauna im Litoral und Benthal von King George (Südshetlandinseln, Antarktis) / M. Rauschert. - IV. Untersuchungen zum Helminthenbefall und zur Nahrung verschiedener Tiergruppen / K. Feiler. - , Zusammenfassung in englischer, deutsche und russischer Sprache , Teilweise in kyrillischer Schrift
    Location: MOP - must be ordered
    Location: MOP - must be ordered
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  • 7
    Call number: O 1590(52) / Regal 28/1
    In: Meddelelse
    Type of Medium: Series available for loan
    Pages: 28 S.
    ISBN: 8774500376
    Series Statement: Meddelelse / Geodaetisk Institut 52
    Location: Magazine - must be ordered
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  • 8
    Call number: O 1590(53) / Regal 28/1
    In: Meddelelse
    Type of Medium: Series available for loan
    Pages: 61 S.
    ISBN: 8750328379
    Series Statement: Meddelelse / Geodaetisk Institut 53
    Location: Magazine - must be ordered
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  • 9
    Call number: D 2025/1-3 / Keller
    Type of Medium: Dissertations
    Pages: getr. Zählung
    Location: Magazine - must be ordered
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  • 10
    Call number: S 91.0718(166/167) / Regal 44/3-4
    In: Procès-verbaux des ... séances de la Commission Géodésique Suisse
    Type of Medium: Series available for loan
    Pages: 20 S.
    Location: Magazine - must be ordered
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  • 11
    Monograph non-lending collection
    Monograph non-lending collection
    Buenos Aires
    Call number: Q 764 / Regal 51
    Type of Medium: Monograph non-lending collection
    Pages: 254 S. , zahlr. Kt.
    Location: Magazine - must be ordered
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  • 12
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: Q 745(2) / REgal 51 ; H G 5568/2
    In: Das Antlitz der Erde
    Type of Medium: Monograph available for loan
    Pages: IV, 704 S. : Ill., Kt.
    Location: Magazine - must be ordered
    Location: Pendulum room
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  • 13
    Series available for loan
    Series available for loan
    Berlin : Nationalkomitee für Geodäsie und Geophysik der Deutschen Demokratischen Republik
    Associated volumes
    Call number: MOP Per 581(3/48) ; ZSP-319/C-48
    In: Geodätische und geophysikalische Veröffentlichungen : Reihe 3, Physik der festen Erde, Heft 48
    Type of Medium: Series available for loan
    Pages: 245 Seiten , Illustrationen
    ISSN: 0435-6187
    Series Statement: Geodätische und geophysikalische Veröffentlichungen : Reihe 3, Physik der festen Erde 48
    Language: German
    Note: Inhaltsverzeichnis Vorwort Zusammenfassungen 1. Problemstellung 2. Terrestrische Refraktion in der Grenzschicht der Atmosphäre 2.1. Lichtausbreitung und Refraktionskoeffizient 2.2. Vertikales Temperaturprofil in der Grenzschicht der Atmosphäre 2.3. Meteorologische Prozesse in der Grenzschicht Antarktikas 2.4. Terrestrische Refraktion Und vertikales Temperaturprofil über polaren Schnee- und Eisflächen (Literaturübersicht) 3. Terrestrische Refraktion bei der trigonometrischen Höhenbestimmung 3.1. Formeln 3.2. Technische Realisierung 3.3. Meßprogramm 3.3.1. Lagemessungen 3.3.2. Streckenbestinunungen für die Refraktionsuntersuchungen 3.3.3. Höhenbestimmungen 3.3.3.1. Nivellements 3.3.3.2. Vertikale Eisbewegung 3.3.3.3. Höhenübertragung auf den Mast 3.3.3.4. Genauigkeit der Höhenbestimmung 3.3.4. Relief der Schneeoberfläche 3.3.5. Messung der Zenitwinkel 3.3.5.1. Beobachtungsprogramm 3.3.5.2. Anzahl der Beobachtungen 3.3.5.3. Dauer und Synchronität der Beobachtungen 3.3.6. Elektrooptische Streckenmessung 3.3.6.1. Meßprogramm 3.3.6.2. Gerätetechnische Parameter 3.4. Beobachtungsfehler 3.4.1. Mittlerer Fehler der Streckenmessung 3.4.2. Mittlere Beobachtungsfehler der Zenitwinkel 3.4.3. Mittlere Fehler des berechneten Höhenwinkels A0, B0 für RK = 0 auf Grund der Beobachtungsfehler 3.4.4. Mittlere Fehler der berechneten Refraktionswinkel und der Refraktionskoeffizienten auf den Endpunkten der Linien auf Grund der Beobachtungsfehler 3.4.5. Mittlere Fehler des Refraktionskoeffizienten RKM auf Grund der Beobachtungsfehler 3.5. Mittlere Refraktionskoeffizienten RKM 3.6. Refraktionskoeffizienten RKA und RKB der einzelnen Visuren 3.7. Differenz der Refraktionswinkel (Refraktionskoeffizienten) bei gegenseitigen gleichzeitigen Beobachtungen 3.8. Geschlossene Dreiecke 4. Thermische Struktur der eisnahen Luftschicht und terrestrische Refraktion 4.1. Meßprogramm und Datenverarbeitung 4.1.1. Geräte 4.1.2. Meßprogramm 4.1.3. Datenverarbeitung 4.2. Meteorologische Verhältnisse im Maßgebiet 4.2.1. Station Molodeznaja 4.2.2. Meßfeld (Punkte 1 - 3)· 4.3. Vertikales Temperaturprofil in der Schicht 0 - 6 m über dem Inlandeis 4.3.1. Form der Temperaturprofile 4.3.2. Ausgewählte Tagesgänge der vertikalen Temperaturgradienten 4.3.3. Statistische Analyse der Temperaturgradienten 4.3.3.1. Empirische Verteilungsfunktionen 4.3.3.2. Mittlerer Jahres- und Tagesgang 4.3.3.3. Räumliche Unterschiede bei gleichzeitigen Messungen 4.3.4. Korrelation mit meteorologischen Parametern 4.3.5. Berechnung von integralen Temperaturgradienten aus wirksamen Refraktionskoeffizienten 4.4. Berechnung von lokalen Refraktionskoeffizienten aus dem vertikalen Temperaturprofil 4.4.1. Ausgewählte Tagesgänge der lokalen Refraktionskoeffizienten 4.4.2. Statistische Analyse der lokalen Refraktionskoeffizienten 4.4.2.1. Empirische Verteilungsfunktionen 4.4.2.2. Mittlerer Jahres- und Tagesgang 4.4.3. Korrelation mit meteorologischen Parametern 4.5. Vergleich zwischen geodätischen und lokalen meteorologischen Refraktionskoeffizienten 4.6. Multiple Regression zwischen dem wirksamen Refraktionskoeffizient und meteorologischen Parametern 4.6.1. Schätzung des wirksamen Refraktionskoeffizienten 4.6.2. Schätzung der Differenz des wirksamen Refraktionskoeffizienten von Stand- und Zielpunkt 4.7. Näherungsweise Lösung des FEARNLEY-Integrals und Korrelation mit geodätischen Refraktionskoeffizienten 4.7.1. Beschreibung des Rechenverfahrens 4.7.2. Vergleich zwischen RK und RP, RM, RF und RJ 4.7.3. Übersicht über die relativen Abweichungen 4.8. Abhängigkeit der Differenz der Refraktionswinkel bei gleichzeitigen gegenseitigen Beobachtungen von meteorologischen Elementen 5. Schlußbemerkungen 6. Literaturverzeichnis
    Location: MOP - must be ordered
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  • 14
    Series available for loan
    Series available for loan
    Associated volumes
    Call number: O 2853(17) / Mag.38
    In: Rapport de la ... session
    Type of Medium: Series available for loan
    Pages: 238 S.
    ISBN: 9282221911
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  • 15
    Monograph available for loan
    Monograph available for loan
    Leningrad : Nedra
    Call number: G 2708 / C3
    Type of Medium: Monograph available for loan
    Pages: 311 S.
    Location: Magazine - must be ordered
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  • 16
    Call number: S 91.0236(M-28) / Regal 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
    Type of Medium: Series available for loan
    Pages: 184 S.
    ISBN: 8388765353
    Series Statement: Publications of the Institute of Geophysics, Polish Academy of Sciences : M, Miscellanea 28 = 363
    Classification:
    Geophysics
    Location: Magazine - must be ordered
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  • 17
    Monograph available for loan
    Monograph available for loan
    Washington : Gov. print. off
    Call number: Q 938 / Regal 51
    Type of Medium: Monograph available for loan
    Pages: 166 S. : Ill.
    Series Statement: Bulletin / U.S. Department of Agriculture. Weather Bureau 1 = 267 [d. Gesamtwerkes]
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  • 18
    Call number: 4707/1 / Regal 13/5
    In: Siebenstellige trignometrische Tafel für Berechnungen mit der Rechenmaschine
    Type of Medium: Monograph available for loan
    Pages: 160 S.
    Location: Magazine - must be ordered
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  • 19
    Call number: 4707/2 / Regal 13/5
    In: Siebenstellige trignometrische Tafel für Berechnungen mit der Rechenmaschine
    Type of Medium: Monograph available for loan
    Pages: S. 161-336
    Location: Magazine - must be ordered
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  • 20
    Call number: MOP Per 581 ; MOP Per 581(1/8) ; ZSP-319/A-1(Sonderheft) ; ZSP-319/A-1(Sonderheft, 2. Ex.)
    In: Geodätische und geophysikalische Veröffentlichungen : Reihe 1, Heft 8, Sonderheft 1
    Type of Medium: Series available for loan
    Pages: 107 Seiten , Illustrationen
    Edition: Sonderheft des NKSCAR der DDR
    Series Statement: Geodätische und geophysikalische Veröffentlichungen : Reihe 1 8
    Language: German , English
    Note: Inhalt: I. Zoologische Untersuchungen im Gebiet der sowjetischen Antarktisstation "Bellinghausen" / R. BANNASCH und K. ODENING. - II. Deuterium- und 18O-Variationen in Seen der Schirmacher-Oase (Ostantarktika) / W. RICHTER und G. STRAUCH. - III. Stable isotope investigations in Antarctica / H. SCHÜTZE, G. STRAUCH, K. WETZEL. - IV. The influence of degradation processes on the isotopic composition of Antarctic precipitation / R. DER. - V. Sommerliche Eisvariationen in der Olaf-Prydz-Bucht / H. GERNANDT. - VI. Zur Geologie des nördlichen Teils des Neptune Range / Pensacola-Gebirges (Antarktika) / W. WEBER und L. V. FEDOROV. - VII. Beobachtungen am Krill (Euphausia superba DANA) im atlantischen Sektor der Antarktis in der Sommersaison 1978 und 1979 / S. HOLZLÖHNER. - VIII. Forschungsreise eines Zubringertrawlers in die Antarktis / G. GUBSCH und U. HOFFMANN.
    Location: MOP - must be ordered
    Location: MOP - must be ordered
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  • 21
    Call number: S 91.0236(M-24) / Mag. 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
    Type of Medium: Series available for loan
    Pages: 424 S.
    ISBN: 8388765124
    Series Statement: Publications of the Institute of Geophysics, Polish Academy of Sciences : M, Miscellanea 24 = 340
    Classification:
    Geophysical Exploration, Geophysical Prospecting
    Location: Magazine - must be ordered
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  • 22
    Call number: S 98.0553(1) / Mag. 38
    In: Rapport du directeur sur l'activité et la gestion du Bureau international des Poids et Mesures (BIPM)
    Type of Medium: Series available for loan
    Pages: 199 S.
    ISBN: 9282221784
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  • 23
    Series available for loan
    Series available for loan
    Warszawa : Inst. Geofizyki Polskiej Akad. Nauk
    Associated volumes
    Call number: S 91.0236(B-24) / Regal 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
    Type of Medium: Series available for loan
    Pages: 211 S.
    ISBN: 8388765086
    Series Statement: Publications of the Institute of Geophysics, Polish Academy of Sciences : B, Seismology 24 = 336
    Classification:
    Geophysics
    Language: English
    Location: Magazine - must be ordered
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  • 24
    Monograph available for loan
    Monograph available for loan
    Paris
    Call number: M 03.0218 / Regal 12
    Type of Medium: Monograph available for loan
    Pages: S. 186 - 235
    Series Statement: Bulletin Mensuel de la Société Linnéenne de la Seine Maritime 11, N. 12
    Location: Magazine - must be ordered
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  • 25
    Call number: G 2688 / C3
    Type of Medium: Monograph available for loan
    Pages: 130 S.
    Location: Magazine - must be ordered
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  • 26
    Call number: S 03.0313(10) / Regal 38
    In: Rapport de la ... session = Report of the ... meeting
    Type of Medium: Series available for loan
    Pages: 208 S.
    ISBN: 9282221970
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  • 27
    Series available for loan
    Series available for loan
    Warszawa : Inst. Geofizyki Polskiej Akad. Nauk
    Associated volumes
    Call number: SR 91.0236(B-32) / Regal 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
    Type of Medium: Series available for loan
    Pages: 109 S.
    ISBN: 8388765345
    Series Statement: Publications of the Institute of Geophysics, Polish Academy of Sciences : B, Seismology 32 = 362
    Classification:
    Seismology
    Language: English
    Location: Magazine - must be ordered
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  • 28
    Call number: O 1590(45) / Regal 28/1
    In: Meddelelse
    Type of Medium: Series available for loan
    Pages: 26 S.
    ISBN: 8774500007
    Series Statement: Meddelelse / Geodaetisk Institut 45
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  • 29
    Series available for loan
    Series available for loan
    Leipzig : Akad. Verl.-Ges.
    Associated volumes
    Call number: O 1590(1-13) / Regal 28/1
    In: Meddelelse
    Type of Medium: Series available for loan
    Pages: S. [402] - 412
    Series Statement: Meddelelse / Geodætisk Institut, København, Danmark 1
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  • 30
    Monograph available for loan
    Monograph available for loan
    Berlin : Springer
    Call number: 600/2 / Regal 12
    Type of Medium: Monograph available for loan
    Pages: VIII, 320 S.
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  • 31
    Call number: S 94.0254(65) / Regal 35
    In: Reports on geodesy
    Type of Medium: Series available for loan
    Pages: 296 S.
    ISBN: 8385287647
    Series Statement: Reports on geodesy 65 = 2003,2
    Location: Magazine - must be ordered
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  • 32
    Series available for loan
    Series available for loan
    Warszawa : Inst. Geofizyki Polskiej Akad. Nauk
    Associated volumes
    Call number: S 91.0236(B-34) / Regal 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
    Type of Medium: Series available for loan
    Pages: 207 S.
    ISBN: 8388765396
    Series Statement: Publications of the Institute of Geophysics, Polish Academy of Sciences : B, Seismology 34 = 367 : monograph volume
    Classification:
    Seismology
    Language: English
    Location: Magazine - must be ordered
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  • 33
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: Q 745(3,2) / Regal 51 ; H G 5568/3,2
    In: Das Antlitz der Erde
    Type of Medium: Monograph available for loan
    Pages: IV, 789 S., 5 Bl. : Ill., Kt.
    Location: Magazine - must be ordered
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  • 34
    Call number: S 91.0470(90) / Mag.38
    In: Procès-verbaux des séances
    Type of Medium: Series available for loan
    Pages: 159 S.
    ISBN: 928222192X
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  • 35
    Series available for loan
    Series available for loan
    Warszawa : Inst. Geofizyki Polskiej Akad. Nauk
    Associated volumes
    Call number: S 91.0236(B-27) / Mag. 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
    Type of Medium: Series available for loan
    Pages: 180 S.
    ISBN: 8388765116
    Series Statement: Publications of the Institute of Geophysics, Polish Academy of Sciences : B, Seismology 27 = 339 : monographic volume
    Classification:
    Seismology
    Language: English
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  • 36
    Series available for loan
    Series available for loan
    Associated volumes
    Call number: S 94.0423(8) / Mag. 38
    In: Rapport de la ... session = Report of the ... meeting
    Type of Medium: Series available for loan
    Pages: 91 S.
    ISBN: 9282221954
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  • 37
    Series available for loan
    Series available for loan
    Warszawa : Inst. Geofizyki Polskiej Akad. Nauk
    Associated volumes
    Call number: S 91.0236(D-60) / Mag. 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
    Type of Medium: Series available for loan
    Pages: 91 S.
    ISBN: 838876523X
    Series Statement: Publications of the Institute of Geophysics, Polish Akademy of Sciences : D, Physics of the atmosphere 60 = 351
    Language: English
    Location: Magazine - must be ordered
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  • 38
    Monograph available for loan
    Monograph available for loan
    Berlin : Nationalkomitee für Geodäsie und Geophysik der DDR bei der Deutschen Akademie der Wissenschaften
    Associated volumes
    Call number: MOP 34587 ; MOP Per 581(1/3) ; ZSP-319/A-3
    In: Geodätische und geophysikalische Veröffentlichungen : Reihe 1, Nr. 3
    Type of Medium: Monograph available for loan
    Pages: 48 Seiten
    Series Statement: Geodätische und geophysikalische Veröffentlichungen : Reihe 1 3
    Language: English
    Location: MOP - must be ordered
    Location: MOP - must be ordered
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  • 39
    Series available for loan
    Series available for loan
    Sevres
    Associated volumes
    Call number: S 98.0553(4) / Mag. 38
    In: Rapport du directeur sur l'activité et la gestion du Bureau international des Poids et Mesures (BIPM)
    Type of Medium: Series available for loan
    Pages: 239 S.
    ISBN: 9282222012
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  • 40
    Monograph available for loan
    Monograph available for loan
    Berlin : Pormetter
    Call number: Q 932 / Regal 51 ; MOP 2731 ; AWI PY-4066-13
    Type of Medium: Monograph available for loan
    Pages: 56 S. : Ill.
    Edition: Sonderabdr.
    Location: Magazine - must be ordered
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  • 41
    Series available for loan
    Series available for loan
    Berlin : Nationalkomitee für Geodäsie und Geophysik der Deutschen Demokratischen Republik
    Associated volumes
    Call number: MOP Per 581(3/40) ; ZSP-319/C-40 ; ZSP-319/C-40(2.Ex.)
    In: Geodätische und Geophysikalische Veröffentlichungen : Reihe 3, Physik der festen Erde, Heft 40
    Type of Medium: Series available for loan
    Pages: 68 Seiten , Illustrationen
    ISSN: 0435-6187
    Series Statement: Geodätische und Geophysikalische Veröffentlichungen : Reihe 3, Physik der festen Erde 40
    Language: German , Russian
    Note: Inhaltsverzeichnis Summary, Rezjume 1. Einleitung 2. Das Bewegungsverhalten von Eismassen, seine Untersuchung und Modellierung 2.1. Zum Modellbegriff 2.2. Typische Eismassen und ihr Bewegungsverhalten 2.2.1. Zur Theorie der Eisbewegung 2.2.2. Gletscher 2.2.3. Schelfeis und Eiskappe 2.3. Die Ermittlung von Eisbewegungen durch geodätische Verfahren 2.3.1. Die Vorplanung der Messungen 2.3.2. Die Durchführung der Messungen 2.3.3. Reduktion der Beobachtungen 2.3.4. Berechnung der Eisbewegungen 2.4. Das trendbehaftete vektorielle Zufallsfeld - Modell zur Beschreibung des Geschwindigkeitsfeldes einer Eismasse - in der Theorie stochastischer Prozesse 2.4.1. Definition des Vektorfeldes 2.4.2. Das Geschwindigkeitsfeld einer Eismasse - trendbehaftetes vektorielles Zufallsfeld 2.4.3. Definition eines vektoriellen Zufallsfeldes 2.4.4. Wahrscheinlichkeitsdichte und Verteilungsfunktion 2.4.5. Die Momente und die Korrelationsfunktionen 2.4.6. Vektorielle Zufallsfelder mit Hormalverteilungsgesetz 2.4.7. Homogene und isotrope vektorielle Zufallsfelder 2.4.8. Das Ergodenproblem 3. Das Konzept der Kollokation und seine Anwendung auf die Bearbeitung von Eisbewegungsmessungen 3.1. Zur Theorie der Kollokation 3.1.1. Das Kollokationsmodell von Moritz [40] 3.1.2. Nichtlineare Prädiktion nach Grafarend [12] 3.1.3. Kollokation von Vektorgrößen 3.2. Analyse und Bearbeitung des Datenmaterials 3.2.1. Die Trendbestimmung 3.2.2. Die Analyse des Zufallsfeldes 3.3. Das Kollokationsmodell bei der Bearbeitung von Eisbewegungsmessungen 3.3.1. Zuordnung und Interpretation der Größen 3.3.2. Zur zeitlichen Variation des Geschwindigkeitsfeldes einer Eismasse 3.3.3. Kollokation mit den ursprünglichen reduzierten Beobachtungen 4. Praktische Untersuchungen 4.1. Geschwindigkeitsquerprofile des Fedtschenko-Gletschers (Pamir) 4.2. Geschwindigkeitslängsprofil des Kongsvegen-Gletschers (Spitzbergen) 4.3. Geschwindigkeitslängsprofil des Hays-Gletschers (Antarktika) 4.4. Geschwindigkeitsquerprofil des Ross-Schelfeises (Antarktika) 4.5. Vergleich mit früheren Untersuchungen zur Abschätzung von Geschwindigkeitskorrelationen natürlicher Eismassen 5. Zusammenfassung 6. Literaturverzeichnis , Zusammenfassung in englischer und russischer Sprache
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  • 42
    Call number: MOP Per 581(3/5) ; ZSP-319/C-5
    In: Geodätische und Geophysikalische Veröffentlichungen : Reihe 3, Physik der festen Erde, Nr. 5
    Type of Medium: Series available for loan
    Pages: 112 Seiten , Illustrationen, Karten , 2 Beilagen
    ISSN: 0435-6187
    Series Statement: Geodätische und Geophysikalische Veröffentlichungen : Reihe 3, Physik der festen Erde 5
    Language: German
    Note: Beilage unter dem Titel: Eisbewegung Mirny - 100.km , Beilage unter dem Titel: Trigonometrisches Netz Mirny 1962 〈1 : 100 000〉 , Inhaltsverzeichnis Vorwort Einführung 1. Aufgabenstellung 2. Beschreibung des Arbeitsgebietes 3· Frühere geodätische Arbeiten im Expeditionsgebiet 4. Expeditionsverlauf 5· Messungen zur Bestimmung der Eisbewegung 5.1. Die trigonometrischen Arbeiten Mirny - 100. km 5.1.1. Technische Ausrüstung und Teilnehmer 5.1.2. Geodätische Instrumente 5.1.3. Erste Beobachtung der trigonometrischen Kette 5.1.4. Zweite Beobachtung der trigonometrischen Kette 5.1.5. Genauigkeiten 5.1.5.1. Richtungen und Zenitwinkel 5.1.5.2. Azimute 5.1.5.3. Streckenmessung 5.1.6. Berechnung der Koordinaten und Höhen 5.1.6.1. Lagemessung 5.1.6.1.1. 1. Beobachtung (2.4.1962) 5.1.6.1.2. 2. Beobachtung (10.11.1962) 5.1.6.2. Höhenmessung 5.1.6.2.1. 1. Beobachtung (2.4.1962) 5.1.6.2.2. 2. Beobachtung (10.11.1962) 5.1.7. Auswertung der Ergebnisse (Horizontale und vertikale Eisbewegung) 5.2. Eisbewegung im Stationsgebiet Mirny 6. Untersuchung der trigonometrischen und nivellitischen Refraktion 6.1. Aufgabenstellung 6.2. Trigonometrische Messungen 6.2.1. Maßanordnung 6.2.2. Durchführung der Beobachtungen 6.2.3. Ergebnisse der trigonometrischen Messungen 6.3. Nivellitische Messungen 6.3.1. Maßanordnung 6.3.2. Durchführung der Beobachtungen 6.3.3. Ergebnisse der nivellitischen Messungen 6.4. Zusammenfassung 7. Versuch zur Durchführung eines motorisierten Nivellements 7.1. Technische Ausrüstung 7 .2. Durchführung der Messungen 7.3. Ergebnisse 8. Literatur
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  • 43
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    Call number: S 91.0470(76) / Mag. 38
    In: Procès-verbaux des séances
    Type of Medium: Series available for loan
    Pages: 215 S.
    ISBN: 9789282222331
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  • 44
    Call number: S 90.1032(58)
    In: Veröffentlichungen der Bayerischen Kommission für die Internationale Erdmessung der Bayerischen Akademie der Wissenschaften
    Type of Medium: Series available for loan
    Pages: 274 S.
    ISBN: 3769696212
    Series Statement: Veröffentlichungen der Bayerischen Kommission für die Internationale Erdmessung bei der Bayerischen Akademie der Wissenschaften : Astronomisch-geodätische Arbeiten 58
    Language: English
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  • 45
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    Warszawa : Inst. Geodezji Wyzsej i Astronomii Geodezyjnej Politechniki Warszawskiej
    Associated volumes
    Call number: S 94.0254(89) / Regal35
    In: Reports on geodesy
    Type of Medium: Series available for loan
    Pages: 448 S.
    ISBN: 9788385287889
    Series Statement: Reports on geodesy 89 = 2010, 2
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  • 46
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    Call number: S 91.0470(77) / Mag. 38
    In: Procès-verbaux des séances
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    Pages: 267 S.
    ISBN: 9789282222386
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  • 47
    Call number: S 91.0718(178/179) / 44/3-4
    In: Procès-verbaux des ... séances de la Commission Géodésique Suisse
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    Pages: 18 S.
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  • 48
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    Call number: S 91.0470(78) / Mag. 38
    In: Procès-verbaux des séances
    Type of Medium: Series available for loan
    Pages: 201 S.
    ISBN: 9789282222447
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  • 49
    Call number: MOP 12884/3 / DG ; Q 1566/3 / Regal 12/6
    In: Wissenschaftliche Ergebnisse der deutschen Grönland-Expedition Alfred Wegener 1929 und 1930/1931
    Type of Medium: Monograph available for loan
    Pages: VII, 270 S. : Ill., graph. Darst., Kt.
    Series Statement: Wissenschaftliche Ergebnisse der deutschen Grönland-Expedition Alfred Wegener 1929 und 1930/1931 ; Bd. 3
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  • 50
    Call number: Z 1079(40-46) / Mag. 31-32
    In: Geologie
    Type of Medium: Journal available for loan
    Pages: 66 S. , Ill., graph. Darst., Kt.
    Series Statement: Geologie : Beiheft 40
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  • 51
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    Call number: M 10.0044/2
    In: Bruch- und Fließ-Formen der technischen Mechanik und ihre Anwendung auf Geologie und Bergbau
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    Pages: 22 S.
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  • 52
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    Call number: M 10.0044/3 / Regal 12
    In: Bruch- und Fließ-Formen der technischen Mechanik und ihre Anwendung auf Geologie und Bergbau
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    Pages: 88 S.
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  • 53
    Call number: O 2069/10 / Mag. 31-32
    In: Geologie
    Type of Medium: Journal available for loan
    Pages: 66 S. , Ill., graph. Darst., Kt.
    Series Statement: Geologie : Beiheft 27
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  • 54
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    Budapest : Geological Inst. of Hungary
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    Call number: S 03.0517(57) / Keller 36/5
    In: Geologica Hungarica
    Type of Medium: Series available for loan
    Pages: 187 S. : Ill., graph. Darst., Kt.
    Series Statement: Geologica Hungarica : series palaeontologica 57
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  • 55
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    Budapest : Geological Inst. of Hungary
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    Call number: S 03.0517(58) / Keller 36/5
    In: Geologica Hungarica
    Type of Medium: Series available for loan
    Pages: 300 S. : Ill., graph. Darst., Kt.
    ISBN: 9789636712785
    Series Statement: Geologica Hungarica : series palaeontologica 58
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  • 56
    Call number: S 97.0188(23) / Mag. 38
    In: Comptes rendus des séances de la ... Conférence Générale des Poids et Mesures (CGPM)
    Type of Medium: Series available for loan
    Pages: 539 S.
    ISBN: 9789282222362
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  • 57
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    Warszawa : Inst. Geodezji Wyzsej i Astronomii Geodezyjnej Politechniki Warszawskiej
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    Call number: S 94.0254(87) / Regal 35
    In: Reports on geodesy
    Type of Medium: Series available for loan
    Pages: 448 S.
    ISBN: 9788385287865
    Series Statement: Reports on geodesy 87 = 2009, 2
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  • 58
    Call number: S 94.0254(86) / Regal 35
    In: Reports on geodesy
    Type of Medium: Series available for loan
    Pages: 128 S.
    ISBN: 9788385287858
    Series Statement: Reports on geodesy 86 = 2009, 1
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  • 59
    Call number: S 94.0254(88) / Regal 35
    In: Reports on geodesy
    Type of Medium: Series available for loan
    Pages: 120 S.
    ISBN: 9788385287872
    Series Statement: Reports on geodesy 88 = 2010, 1
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  • 60
    Call number: AWI E2-11-0018 ; AWI PY-1955-13
    Type of Medium: Monograph available for loan
    Pages: VII, 630 S. : Ill., Kt. , 2 Kt.
    Language: English
    Note: Kt. u.d.T.: Part of Franz Josef Archipelago surveyed by the Ziegler Polar Expedition 1903-4-5 〈1 : 600.000〉 ; Map of Franz Josef Archipelago compiled from surveys of the Ziegler Polar Expeditions 1901--02, 1903-5, and from information published by Payer (1872-74), Leigh Smith (1880-81), Jackson (1894-97), Nansen (1895-96), Wellman (1898-99), the Duke of the Abruzzi (1899-1900) 〈1 : 750.000〉 , Contents: Introduction by Anthony Fiala. - Section A - Magnetic Observations and Reductions. - Section B - Notes and Sketches of the Auroræ Borealis. - Section C - Meteorological Observations and Compilations. - Section D - Tidal Observations and Reductions. - Section E - Astronomic Observations and Reductions. - Section F - Map construction and survey work
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  • 61
    Call number: S 91.0718(180/181) / 44/3-4
    In: Procès-verbaux des ... séances de la Commission Géodésique Suisse
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    Pages: 20 S.
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  • 62
    Call number: MOP 12884/1 / DG ; Q 1566/1 / Regal 12/6
    In: Wissenschaftliche Ergebnisse der deutschen Grönland-Expedition Alfred Wegener 1929 und 1930/1931
    Type of Medium: Monograph available for loan
    Pages: XII, 198 S. : Ill., 1 Portr., graph. Darst., Kt. + 1 Kt.-Beil.
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  • 63
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    Call number: S 98.0553(11) / Mag. 38
    In: Rapport du directeur sur l'activité et la gestion du Bureau international des Poids et Mesures (BIPM)
    Type of Medium: Series available for loan
    Pages: 371 S.
    ISBN: 9789282222416
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  • 64
    Call number: S 91.0470(79) / Mag. 38
    In: Procès-verbaux des séances
    Type of Medium: Series available for loan
    Pages: 249 S.
    ISBN: 9789282222454
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  • 65
    Call number: MOP 12884/2 / DG ; Q 1566/2 / Regal12/6
    In: Wissenschaftliche Ergebnisse der deutschen Grönland-Expedition Alfred Wegener 1929 und 1930/1931 ; Bd. 2
    Type of Medium: Monograph available for loan
    Pages: 160 S., 3 gef. Bl. : Ill., graph. Darst., Kt.
    Series Statement: Wissenschaftliche Ergebnisse der deutschen Grönland-Expedition Alfred Wegener 1929 und 1930/1931 ; Bd. 2
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  • 66
    Call number: S 91.0718(184/185) / 44/3-4
    In: Procès-verbaux des ... séances de la Commission Géodésique Suisse
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    Pages: 28 S.
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  • 67
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    Hanover, N.H. : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-202-350
    In: Research report / Cold Regions Research and Engineering Laboratory, 350
    Type of Medium: Series available for loan
    Pages: iv, 27 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 350
    Language: English
    Note: CONTENTS: Abstract. - Preface. - Introduction. - Sample preparation. - Apparatus and testing procedure. - Test results. - Uniaxial strength. - Initial tangent and 50% strength moduli. - Specific energy. - Discussion. - Testing method. - Compressive strength. - Tensile strength. - Ductile and brittle fracture.. - Initial tangent and 50% stress moduli. - Specific energy. - Conclusions and recommendations. - References. - Appendix A: Description of soil and calculations. - Appendix B: Description of the LVDT and averaging circuits. - Appendix C: Determination of strain in the neck section of a dumbbell specimen.
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  • 68
    Call number: ZSP-202-348
    In: Detecting structural heat losses with mobile infrared thermography, Part III
    In: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command, 348
    Description / Table of Contents: During the winter of 1973 - 74 a mobile infrared thermography system was used to survey the USA CRREL building at Hanover, New Hampshire. This report provides a description of excessive heat losses at several locations around the building. This report also discusses the need to carefully monitor meteorological conditions before starting a survey of a building exterior to determine if solar radiation decay from the building surface might interfere with thermographic analysis by masking the heat emanating from within the building.
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    Pages: ii, 9 S. : Ill.
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 348
    Language: English
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  • 69
    Call number: ZSP-202-347
    In: Research report / Cold Regions Research and Engineering Laboratory, 347
    Description / Table of Contents: CONTENTS: Abstract. - Preface. - Introduction. - Experimental. - Results and discussion. - Applications. - Literature cited.
    Description / Table of Contents: Chemical analysis of century-old ice from continuous 5 to 7 year intervals of three ice cores from south and central Greenland (Dye 3, Milcent and Crete) show maximum concentrations of Na, Mg,Ca, K, and Al during early spring and minimum concentrations during late summer and early fall. Peak spring values are as much as 10 times greater than fall values. Because of the large seasonal chemical variations, samples used for depth-age or annual deposition rate studies must represent accumulation from exactly one year or whole multiples of a year. The seasonal chemical variations seem promising as a new method of defining annual layers and thus dating old ice cores.
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    Pages: iii, 5 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 347
    Language: English
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  • 70
    Call number: ZSP-202-346
    In: Research report / Cold Regions Research and Engineering Laboratory, 346
    Description / Table of Contents: CONTENTS: Abstract. - Preface. - USA CRREL project and personnel involvement. - Part I. Introduction. - Background. - Literature review. - Part II. CRREL investigations from 1970 - 1974. - Initial literature survey (1970). - Oil detection kit development. - Survey of Cape Simpson, Alaska, natural crude oil seepages (1970). - Haines-Fairbanks military pipeline investigations (1971-1973). - Barrow investigations (1970-1974). - Fairbanks and Fox investigations. - Germination studies. - Physiological studies. - Dispersant studies. - Microbiological investigations. - Field investigations of accidental petroleum losses. - Part III. Recent related literature. - Part IV. Conclusions and recommendations. - USA CRREL reports, publications and presentations on Alaska oil spill research. - Literature cited.
    Description / Table of Contents: Knowledge concerning the biological effects of oil pollution on arctic and subarctic terrestrial ecosystems is limited. USA CRREL research personnel conducted investigations from 1970 through 1974 to expand information in this field. Objectives were to: 1) define the ecosystems most sensitive to the presence of crude oil or its refined products, 2) quantify and understand the injury response, and 3) establish time frames for manifestation of damage and natural restorative processes in arctic and subarctic regions. This was accomplished through: 1) surveys of natural oil seepages and past accidential spills in the Arctic and Subarctic, 2) initiation of controlled oil spills and 3) detailed laboratory investigations. Results demonstrated that terrestrial oil spills will to some degree be detrimental to both arctic and subarctic plant communities. Degree and longevity of damage will be influenced primarily by the magnitude of the spill, season of occurrence and existing soil moisture content. Rapid recovery of plant communities subjected to spills will occur only if root systems remain relatively unaffected. Damage will be more extensive and long-term when root systems are saturated with oil. Effects of damage will be manifested gradually over several seasons being influenced by winter stresses. Variation does exist in plant species susceptibility. Carex aquatilis, a predominant sedge of the arctic, is markedly resistant to crude oil damage. In the taiga Picea mariana is very susceptible. Plant recovery can be enhanced through the application of fertilizer. Fertilization, in addition to its direct effect on plant nutrition, will stimulate microbial decomposition of crude oil.
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    Pages: vii, 66 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 346
    Language: English
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  • 71
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    Hanover, NH : Corps of Engineers, U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-202-244
    In: Research report
    Description / Table of Contents: CONTENTS: Introduction. - Summer temperature data. - Station network and history. - Parameters for data reduction. - Analysis of summer temperatures. - Temperature trends. - Summer temperatures in the highlands. - Lapse rates for summer temperatures. - Spatial variation of summer temperatures. - Summary. - Literature cited. - Appendix A. - Appendix B. - Appendix C. - Abstract.
    Description / Table of Contents: Annual degree-day summations over bases of 43°F and 50°F in 15-day periods from May through August are given for the period of record for five interior Alaska climatic stations. Average temperature and precipitation data are included. Patterns of summer temperature in interior Alaska are analyzed in terms of historical, elevational and areal differences. Since 1900, summer temperatures show little long-term change but significant short-term changes. In contrast, winter temperatures show considerable fluctuations, which are reflected in mean annual temperatures to a much greater degree than are summer temperature fluctuations. Average summer lapse rates for the 1600 to 3300 and 3300 to 6600-ft levels were 3.4 and 3.7°F/1000 ft, respectively, based on timberline temperature observations and on upper air data from Fairbanks. Correlation analysis of daily and monthly average July temperatures indicates areas of uniformity with respect to temperature variation. This provides information on lowland climatic stations that are representative of highland locations, especially the Yukon-Tanana Uplands
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    Pages: iv, 37 Seiten , Illustrationen, Karten
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 244
    Language: English
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  • 72
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    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
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    Call number: ZSP-202-260
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction and statermnt of problem. - Solution of problem shown in Figure 3. - Solution of problem shown in Figure 4. - The negligibility of the effects of buoyancy and incompressibility of the sealed liquid. - Literature cited.
    Description / Table of Contents: After a brief description of the circumstances which led to the investigation of the title problem and discussion of some related previous investigations, exact solutions are derived for a circular plate which seals an incompressible liquid, is clamped along the boundary and is subjected at an arbitrary point to a lateral concentrated force P. For the case when the plate is covered by a thin liquid layer the solution is obtained in closed form. When this liquid layer is absent, the solution is obtained as an infinite series. The paper concludes with a study of the range of the parameter ([Lambda] a) for which the effort of buoyancy is negligible upon the deflections and stresses in the plate.
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    Pages: iv, 11 Seiten , Illustartionen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 260
    Language: English
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  • 73
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    Hanover, NH : U.S. Army Materiel Command, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-257
    In: Research report
    Description / Table of Contents: CONTENTS: PREFACE. - NOMENCLATURE. - SUMMARY. - INTRODUCTION. - TECHNICAL BACKGROUND. - Rankine-Hugoniot Shock Equations. - The Rayleigh Line. - Release Cross Curves. - Impedance Match Technique for Measuring Hugoniots and Release Isentropes. - EXPERIMENTS. - Sample Materials. - Ottawa Sand. - West Lebanon Glacial Till. - Ice . - Sample Preparation. - Experimental Procedures. - EXPERIMENTAL DATA AND RESULTS. - Ottawa Sand. - West Lebanon Glacial Till. - Ice. - Release Cross Curves. - Dry Ottawa Sand. - Saturated Ottawa Sand. - Ice. - SUMMARY AND RECOMMENDATIONS FOR FUTURE WORK. - REFERENCES.
    Description / Table of Contents: To compute shock wave propagation in frozen soil-water mixtures it is necessary to know a constitutive relation or an equation of state of the medium under consideration. Shock wave techniques provide a powerful tool for the investigation of equations of state at very high stress levels. The stress-volume behavior of frozen soil-water mixtures in the range from 60 to 500 kbar was investigated. Hugoniot data were obtained for Ottawa banding sand (pure quartz sand) and West Lebanon (New Hampshire) glacial till of varying degrees of saturation and for polycrystalline and monocrystalline ice (c-axis oriented in the direction of shock propagation). Release cross curve data were obtained for dry and saturated Ottawa banding sand and for polycrystalline ice. All materials were at an initial temperature of -10°C. In all experiments plane one-dimensional shock waves were used. The Hugoniots and release curves for the soil materials show evidence of a quartz-stishovite phase transition at about 300 kbar. The Hugoniots of single and polycrystalline ice do not differ significantly over the stress range studied - 30 kbar to 300 kbar.
    Type of Medium: Series available for loan
    Pages: vii, 50 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 257
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  • 74
    Monograph non-lending collection
    Monograph non-lending collection
    Wien : Kaiserl.-Königl. Hof- und Staatsdr.
    Associated volumes
    Call number: AWI PY-2344-13
    In: Denkschriften
    Type of Medium: Monograph non-lending collection
    Pages: S. 69 - 292, Taf A - G : graph. Darst.
    Series Statement: Denkschriften / Akademie der Wissenschaften in Wien, Mathematisch-Naturwissenschaftliche Klasse 35, [4]
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  • 75
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-251
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Theory. - Application to ice sheets and ice shelves. - Summary. - Literature cited.
    Description / Table of Contents: An analysis is made of the rate of bubble coalescence in a deforming ice mass. A total strain of at least 8 is required before appreciable coalescence occurs, The analysis has.been applied to deforming ice shelves and ice sheets. No appreciable coalescence is expected in ice shelves but coalescence should occur in ice sheets (or glaciers) if the shear strain rate at the bottom surface is of the order of 0.075/yr or larger. Measurements of bubble concentration are capable of setting limits on paleo-strain rates of the present ice sheets. Bubble migration down temperature gradients presents complications to the study of bubble coalescence.
    Type of Medium: Series available for loan
    Pages: iv, 5 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 251
    Language: English
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  • 76
    Monograph non-lending collection
    Monograph non-lending collection
    Associated volumes
    Call number: AWI PY-1892-13,1
    In: Die internationale Polarforschung 1882 - 1883
    Description / Table of Contents: Inhalt: Vorbericht zur wissenschaftlichen Polarexpedition nach Jan Mayen von dem Leiter der Expedition Corvetten-Capitän Emil Edlen von Wohlgemuth. - 1. Theil Astronomie, bearbeitet von Linenschiffs-Lieutenant Richard Freiherrn Basso von Gödel-Lannoy. - 2. Theil Aufnahme und Beschreibung der Insel Jan Mayen und Beobachtungen über Gletscherbewegung, durchgeführt und bearbeitet von Linienschiffs-Lieutenant Adolf Bobrik von Boldva. - 3 Theil 1. Abtheilung Meteorologie, bearbeitet von Linienschiffs-Lieutenant Adolf Sobieczky. - 2. Abtheilung Temperatur und specifisches Gewicht des Seewassers, bearbeitet von J. Luksch und J. Wolf. - 3. Abtheilung Resultate der chemischen Untersuchungen über die von Jan Mayen mitgebrachten Seewasserproben, bearbeitet von A. Kliemetschek und J. Sobieczky. - 4. Abtheilung Ebbe- und Fluthbeobachtungen, bearbeitet von Linienschiffs-Lieutenant Adolf Bobrik von Boldva.
    Type of Medium: Monograph non-lending collection
    Pages: Getr. Zählung : graph. Darst., Kt.
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  • 77
    Call number: AWI PY-1893-13,2
    In: Report on the proceedings of the United States expedition to Lady Franklin Bay, Grinnell Land
    Type of Medium: Monograph non-lending collection
    Pages: VI, 738 S. : Ill., Kt., graph. Darst.
    Note: CONTENTS: SCIENTIFIC APPENDICES. - 129. Natural History (Mammalia). - 130. Botany. - 131. Ornithology. - 132. Medusae. - 133. Echinodermata, Vermes, Crustacea, and Pteropod Mollusca. - 133a. Trout caught in Lake Alexandra. - 134. Mollusca. - 135. Astronomical observations. - 136. Hydrography. - 137. Sound experiments. - 138. Meteorology. - 138a. Meteors. - 138b. Authorities on Arctic meteorology. - 139. Magnetic reductions by U. S. Coast and Geodetic Survey. - 139a. Magnetic reductions, 1881-'82. - 140. Tidal Observations reduced by U. S. Coast and Geodetic Survey. - 141. Pendulum observations reduced by U. S. Coast and Geodetic Survey. - Index to Vol. II. - METEOROLOGICAL TABLES. - 1-5. Hourly readings of aneroid barometer, August to December, 1881. - 6-30. Hourly readings of mercurial barometer, August, 1881, to August, 1883. - 31. Mean daily barometer, August 8, 1881, to August 8, 1883. - 32. Mean hourly barometer by months, August, 1881, to include July, 1883. - 33. Mean barometer by decades, 1875-'76, 1881-'83. - 34. Mean monthly pressure at various Arctic stations. - 35. Mean monthly pressure at Fort Conger, 1875-'76, 1881-'83. - 36. Mean hourly barometer at Fort Conger for 601 days, and 216 days without the sun. - 37. Mean hourly barometer at Fort Conger for each month of the year in departures. - 38. Diurnal barometer fluctuations at various Arctic stations. - 39. Departures (by months) from mean annual pressure at Fort Conger. - 40. Maxima and minima pressures. - 41. Daily barometric ranges, 1881-'83. - 42. Maxima and minima daily barometric ranges, 1881-'83. - 43. Greatest hourly and daily barometric changes, 1881-'83. - 44-68. Hourly temperature Observations, August, 1881, to August, 1883. - 69. Daily mean temperatures, August 5,1881, to August 8, 1883. - 70. Hourly mean temperatures by months, August, 1881, to July, 1883. - 71. Mean temperatures by decades, 1875-'76, 1881- '83. - 72. Mean monthly temperatures for Arctic Stations north of Kennedy Channel. - 73. Mean monthly temperatures for Arctic stations near Littleton Island. - 74. Mean monthly ranges of temperature, 1875-'76, 1881 -'83. - 75. Mean daily ranges of temperature, 1881-'83. - 76. Maxima, minima, and absolute temperature ranges, 1875-'76, 1881-'83. - 77. Diurnal amplitude of temperatures at various Arctic stations. - 78. Mean diurnal fluctuations of temperature for each month, etc. - 79. Hourly temperature changes of 9°, 1881-'83. - 80. Hours of zero weather, freezing mercury, etc. - 81-104. Moisture of the air by months, August, 1881, to July, 1883. - 105-128. Wind velocity by months, August, 1881, to July, 1883. - 129. Comparative wind velocities at and near Fort Conger. - 130. High winds, 1881-'83. - 131. Frequency and velocity of winds by months, 1881-'83. - 132. Winds of various velocities, 1881-'83. - 133. Hourly and monthly wind resultants, 1881-'83, and storms at Fort Conger. - 134-157. Clouds and rainfall, August, 1881, to July, 1883. - 158. Evaporation of ice and water. - 159. Mean cloudiness by months, 1881-'83. - 160. Hours of rain, snow, etc., 1875-'76, 1881-'83. - 161. Rain and melted snow by months, 1881-'83. - 162. Precipitation by hoar frost, 1881-'82. - 163. Mean daily evaporation, 1881-'82. - 164. Solar and terrestrial radiation observations, 1881-'83. - 165. Differences between maximum black bulb thermometer and ordinary maximum, 1881-'83. - 166. Differences between radiating minimum thermometer and ordinary minimum, 1881-'83. - 167. Means and extremes of maximum solar black bulb, 1881-'83. - 168. Means and extremes of minimum terrestrial observations, 1881-'83. - 169. Monthly means sea temperatures and ice measurements, 1881-'83. - 170. Monthly means sea temperatures at high and low water, 1882-'83. - 171. Sea temperatures and ice measurements, 1881-'83. - 172. Sea temperatures at high and low water, 1882- '83. - 173. Frequency of auroras, 1881-'83. - 174. Pressure, temperature, and humidity, St. Johns to Lady Franklin Bay, 1881. - 175. Wind, weather, and rainfall, St. Johns to Lady Franktin Bay, 1881. - 176. Temperature of the sea, St. Johns to Lady Franklin Bay, 1881. - 177. Barometer observations, Fort Conger to Camp Clay, 1883. - 178. Temperature observations, Fort Conger to Camp Clay, 1883. - 179. Wind, weather, tides, etc., Fort Conger to Camp Clay, 1883. - 180. Barometer observations at Camp Clay, October, 1883, to May, 1884. - 181. Temperature Observations at Camp Clay, October, 1883, to June, 1884. - 182. Wind, weather, etc., at Camp Clay, October, 1883, to June, 1884. - 183. Daily means of atmospheric pressure, August 1,1883, to May, 1884. - 184. Daily means of temperature of air, August, 1883, to June, 1884. - 185. Comparative anemometer readings at Dutch Island and Fort Conger. - 186. Field meteorological Observations. - METEOROLOGICAL CHARTS. - 1,2. Area of high monthly pressure over Northern Hemisphere. - 3,4. Area of low monthly pressure over Northern Hemisphere. - 5. Annual fluctuation of pressure at Fort Conger. - 6. Diurnal fluctuation of pressure at Fort Conger. - 7. Diurnal fluctuation at various Arctic stations, sinmltaneous. - 8. Diurnal fluctuation at various Arctic Stations, local time. - 9. Annual fluctuation of temperature of air at Fort Conger. - 10. Annual inequality in diurnal amplitude of tempernture. - 11. Mean diurnal fluctuation of temperature, 1881-'83.. - 12. Annual fluctuation in wind's direction, 1881-'83. - 13. Diurnal fluctuation in wind's direction, 1881-'83. - 14. Comparative departures of mean temperatures and cloudiness, 1881-'83. - 15,16. Simultaneous weather charts, March 8 and 9, 1883. - 17. Annual curves of solar and terrestrial radiation, 1881-'83. - TERRESTRIAL MAGNETISM. - Introduction. - Observations for local time at Fort Conger, Grinnell Land. - Observations and result for latitude of Fort Conger. - Observations for azimuth of magnetic mark. - Determination of longitude of Fort Conger - by chronometers. - Determination of longitude of Fort Conger - by moon culminations. - Determination of longitude of Fort Conger - by occultations. - Determination of longitude of Fort Conger - by lunar distances. - Resulting longitude of Fort Conger. - Observations and results of the magnetic declination, September, 1881, to August, 1882. - Solar-diurnal variation from first year's series. - Observations and results of hourly series of declinations, July, 1882, to August, 1883. - Recognition and analysis of the disturbances in declination. - Solar-diurnal variation of the declination derived from the hourly series of the second year. - Discussion of the larger disturbances in declination. - Term-day observations of the declination. - Term-hour observations of the declination. - Special term observations. - Measure of the horizontal component of the magnetic force. - Observations of deflections. - Observations of oscillations. - Results for horizontal itensity. - Observations of the magnetic dip. - Hourly series of the dip, October, 1882, to June, 1883. - Results for dip, vertical and total intensity. - Record and description of auroral displays. - Collection of magnetic declinations observed during geographical explorations. - General collection of magnetic observations in the region of approaches to and north of Smith's Sound. - Declination of the magnetic needle at Fort Conger, September 17, 1881, to June 22, 1882. - MAGNETIC CHARTS. - Diurnal variation of the magnetic declination at Fort Conger, September, 1881, to September, 1882. - Solar-diurnal variation of the magnetic declination at Fort Conger, August, 1882, to August, 1883. - Relative frequency of disturbances in declination at Fort Conger, August, 1882, to August, 1883. - Term-day observations at Fort Conger. Magnetic declination East. Plates I, II, III, IV. - Term-hour observations at Fort Conger. Magnetic declination East. Plates V, VI. - TIDAL OBSERVATIONS. - Introductory. - Record of hourly observations. - Recordof observed high and low waters, computed
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  • 78
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    Monograph non-lending collection
    Associated volumes
    Call number: AWI PY-1897-13,1-2
    In: Observations faites aux stations de Sodankylä et de Kultala
    Description / Table of Contents: Table des matières: TOME 1 MÉTÉOROLOGIE. - Introduction. - Observation météorologique. - Pression atmosphérique. - Température de l'air. - Température sur le sol. - Température du sol: 1° à 0,4 m., 2° à 0,8 m. et 3° à 1,6 m. de profondeur. - Humidité de l'air. - Direction et vitesse du vent. - Nébulosité, forme et direction des nuages, hydrométéores. Eau tombée. - Evaporation de l'eau douce. - Température sur le sol et à 6 cm. de profondeur. - Température de l'eau de la rivière. - Remarque diverses; couches des nuages à hauteur différente. - Observations météorologiques de l'année 1883-84 faites à Sodankylä. - Remarques diverses 1883-84. - Observations météorologiques faites à Kultala. - Remarques diverses. - Aperçu général de moyennes mensuelles et de variations diurnes: variation de la pression atmosphérique, de la température de l'air, de la température sur le sol, de l'humidité de l'air, de la vitesse du vent, de la nébulosité et de l'eau tombée. - Fréquence des vents. - Les années 1882 - 83 et 1883 - 84 au point de vue météorologique. - TOME 2 MAGNÉTISME TERRESTRE. - Déterminations magnétiques absolues. - Observations des variations magnétiques. - Réduction des observations en valeurs absolues. - Déterminations des constants pour les instruments de variation à Kultala. - Déterminations magnétiques absolues faites à quelques endroits pendant le voyage. - Remarques sur les tableaux. - Observations mangnétiques 1882-1883. - Déclinaison. - Intensité horizontale. - Intensité verticale. - Observations-termes magnétiques 1882-1883. - Variations des éléments magnétiques pendant les jours termes. - Observations faites de 20 secondes en 20 sec. pendant les jours termes. - Observations magnétiques 1883-1884. - Observations horaires des éléments magnétiques à 5h a. m., 1h p. m. et 9h p. m. temps moyen de Göttingue. - Observations-termes magnétiques 1883-1884. - Variations des éléments magnétiques pendant les jours termes. - Variations des éléments magnétiques observées chaque demi-minute de 8h 30m à 10h 30m p. m. le 1er, 8me, 15me et 22me du chaque mois. - Variations des éléments magnétiques observées chaque demi-minute pendant une heure au soir avant les jour-termes suivantes: 1 janvier de 6h à 7h p.m., 14 janvier 7h-8h p. m., 31 janvier 8h-9h p. m., 14 février 9h-10h p. m., 29 février 10h-11h p. m. et 14 mars 11h-12h p. m. - Perturbations magnétiques observées. - Observations magnétique faites à Kultala. - Tableaux des variations magnétiques diurnes observées pendant les jours sans perturbations, conformément au projet de M. Wild. - Planches. - 1. Courbes représentant les moyennes des variations magnétiques diurnes pendant les jours sans perturbations, conformément au projet de M. Wild. - 2. Suite de courbes précédentes et courbes représentant les moyennes des moyennes précédentes.
    Type of Medium: Monograph non-lending collection
    Pages: Getr. Zählung
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  • 79
    Call number: ZSP-202-338
    In: Detecting structural heat losses with mobile infrared thermography / R.H. Munis, S.J. Marshall and M.A. Bush, Part II
    In: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command, 338
    Description / Table of Contents: CONTENTS: Abstract. - Preface. - Introduction. - Discussion of heat loss survey of six housing units. - Survey of base facilities. - Conclusions. - Literature cited.
    Description / Table of Contents: During the winter of 1973-74 a mobile infrared thermography system was used to survey housing units and base facilities at Pease Air Force Base, Portsmouth, New Hampshire. This report provides both qualitative and quantitative evidence regarding heat flow out of the eave vents of these housing units. Calculations indicate that a significant amount of heat is being lost in this manner due to inadequate attic (cap) insulation. Possible evidence of incomplete ventilation could explain the presence of condensation in the housing units. Analyses of thermograms are presented to show the possible existence of low and high pressure areas around a structure and how they relate to heat loss.
    Type of Medium: Series available for loan
    Pages: iii, 29 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 338
    Language: English
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  • 80
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-345
    In: Research report / Cold Regions Research and Engineering Laboratory, 345
    Description / Table of Contents: CONTENTS: Abstract. - Preface. - List of symbols. - Introduction. - Previous work. - Experimental design. - The radioisotope 22Na. - Description of apparatus. - Experimental procedure. - Correction of profiles. - Assumptions. - Decay correction. - Boundary correction. - Error analysis. - Results. - Salinity data. - Temperature data. - Growth velocity. - Discussion. - Brine and ice properties. - Brine salinity. - Brine density. - Brine volume. - Brine latent heat of freezing. - Brine viscosity, specific heat, and thermal conductivity. - Ice properties. - Theoretical brine expulsion model. - Continuity equations. - Thermal energy equation. - Simplified brine expulsion equations. - Brine expulsion in NaCl ice. - Results. - Discussion. - Gravity drainage in NaCl ice. - Application of results to natural sea ice. - Effective distribution coefficient. - Previous work. - Experimental procedure and results. - Conclusions. - Literature cited. - Appendix A: Profile correction data. - Appendix B: Program "correct" and sample output. - Appendix C: Tabulation of salinity data. - Appendix D: Tabulation of profile data. - Appendix E: Time-ice thickness equations (Runs 2 and 3). - Appendix F: Tabulation of distribution coefficient data.
    Description / Table of Contents: To obtain a better understanding of the desalination of natural sea ice, an experimental technique was developed to measure sequential salinity profiles of a growing sodium chloride ice sheet. Using radioactive 22Na as a tracer, it was possible to determine both the concentration and movement of the brine within the ice without destroying the sample. A detailed temperature and growth history of the ice was also maintained so that the variation of the salinity profiles could be properly interpreted. Since the experimental salinity profile represented a smoothed, rather than a true salinity distribution, a deconvolution method was devised to restore the true salinity profile. This was achieved without any significant loss of end points. In all respects, the salinity profiles are similar to those of natural sea ice. They have a characteristic C-shape, and clearly exhibit the effects of brine drainage. Not knowing the rates of brine expulsion or gravity drainage, the variation of the salinity profiles during the period of ice growth could be explained by either process. To determine the relative importance of the desalination mechanisms, a theoretical brine expulsion model was derived and compared to the experimental data. As input for the model, equations describing the variation of some properties of NaCl brine with temperature were derived. These included the brine salinity, viscosity, specific heat, thermal conductivity, and latent heat of freezing. The theoretical brine expulsion model was derived by performing mass and energy balances over a control volume of NaCl ice. A simplified form of the model, when compared to the experimental results, indicated that brine expulsion was only important during the first several hours of ice growth, and later became a minor desalination process relative to gravity drainage which continued to be the dominant mechanism for the remainder of the study period (up to 6 weeks). The rate of gravity drainage was found to be dependent on the brine volume and the temperature gradient of the ice. As either the brine volume or temperature gradient was increased, the rate of change of salinity due to gravity drainage increased. The equation commonly used to calculate the effective distribution coefficient (Weeks and Lofgren 1967) was modified and improved by taking brine drainage into account. An expression was also derived to give the distribution coefficient at very low growth velocities.
    Type of Medium: Series available for loan
    Pages: vii, 85 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 345
    Language: English
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  • 81
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    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-245
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Snow crystals in Greenland. - Microspherules. - Microspherules in snow and ice-fog crystals. - Concentration and radii of spherules. - Discussion and conclusions. - Literature cited.
    Description / Table of Contents: Spherules found in snow crystals, ice-fog crystals, fallout particles, and fly ash were studied with an electron microscope using the electron diffraction method. The central part of the residues of 1004 specimens of natural snow crystals from Greenland, the United States, and Japan were examined; 14 spherules 0.1 to 1.5? in radius were found among them. The residues of 658 artificial ice-fog crystals formed from water vapor in flue gases of coal-burning electric power plants at Fairbanks, Alaska, were also examined; nine spherules were found. Spherules similar to those found in ice-fog residues were found in furnace-produced fly ash fallout at Fairbanks, Alaska. Electron and optical microscope examination of spherules found in Greenland snow reveals a size distribution of the form dN/d(log r) = Cr-ß where ß approximately 3. The properties of spherules and the mean mass of snow crystals from Greenland are described. The electron microscope study indicated that less than 0.7% of the 1004 snow crystals contained spherules of possible extraterrestrial origin, and that snow crystals are formed mainly on clay mineral particles by heterogeneous nucleation.
    Type of Medium: Series available for loan
    Pages: iv, 10 Seite , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 245
    Language: English
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  • 82
    Call number: Z 94.0251
    Type of Medium: Journal available for loan
    ISSN: 1038-4871
    Language: English
    Location: Magazine - must be ordered
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  • 83
    Series available for loan
    Series available for loan
    Hanover, NH : US Army Materiel Command, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-240
    In: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command, 240
    Description / Table of Contents: A 4-summer hydrologic record from a 1.6 km^2 drainage basin at Barrow, Alaska is analyzed. The watershed, a drained lake basin, is underlain by continuous permafrost within 0.3m of the tundra surface and is covered by ice-wedge polygons and numerous small shallow ponds. Considerable variations from the 20-yr means of summer climate (thaw period 88 days, precipitation 67 mm) are represented in the data: 1963 - cold, extremely wet; 1964 - cold, extremely dry; 1965 - cool, dry; 1966 - cool, wet. Runoff varied greatly from storm to storm, occurring primarily through and over the tundra mat and through an intricate system of polygonal troughs and ponds. As a result of the subdued coastal topography, varying areas (0.3 km^2 to 1.6 km^2) contribute to runoff from different storms. Analyses of hydrographs revealed: 1) lag times generally from 3 to 10 hr; 2) recession constants of about 50 hr, but occasionally as much as 160 hr; and 3) runoff from individual storms between 1 and 70%. About 5% of the thaw season precipitation normally runs off. Comparison of total thaw season precipitation between the U.S. Weather Bureau and a shielded gage located on the watershed indicated no major differences. If "trace" precipitation is considered, only 90% of the actual precipitation may be recorded. Pan evaporation for an average thaw season is about 160 mm and evapotranspiration which is essentially in balance with precipitation is about 60 mm. Conductivity of runoff water varied from 250 [My]mhos during sustained discharge to more than 500 [My]mhos during low flows in dry years. Precipitation chemistry showed no correlation with storm direction. Assuming all winter precipitation runs off, and the data are spatially and temporally representative, about 50% of the measured annual precipitation in this region runs off into the Arctic Ocean.
    Type of Medium: Series available for loan
    Pages: IV, 18 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 240
    Language: English
    Note: CONTENTS: Preface. - Summary. - Introduction. - Regional setting. - Description of watershed. - Climatic record. - Methods. - Precipitation. - Water and air temperatures. - Discharge. - Evaporation and pond levels. - Water chemistry. - Soil thaw. - Results and discussion. - Precipitation. - Runoff. - Evaporation and transpiration. - Water chemistry. - Conclusions. - Literature cited.
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  • 84
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    Series available for loan
    Hanover, NH : U.S. Army Corps of Engineers, Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-250
    In: Research report
    Description / Table of Contents: CONTENTS: Introduction. - Methods. - Results. - Ground and aerial photography. - Hemispherical photography. - Light quality. - Discussion. - Literature cited. - Abstract.
    Description / Table of Contents: Aerial and ground photographs were taken over a 2-year period of sites in the El Verde rain forest to record the consistency of the vegetational patterns in untreated sites and the changes that occurred following gamma irradiation. Four emulsions were used: panchromatic infrared, false color transparency and color transparency. Densitometry was used to evaluate color film and the vegetation response to 3 months of radiation. The color emulsions provided the sharpest indication of damage to vegetation and the succession following treatment. Hemispherical photography of the canopy was evaluated in terms of a canopy cover index defined as percent of light passing through the negative in a 90-degree cone area. Control stations were remarkably constant in all photography, establishing the stability and slow natural changes in rain forest structure. Spectral light measurements within the forest confirmed the predominance of far red shade light. Compared to similar studies on the chronic irradiated forest at Brookhaven National Laboratory the El Verde results were less distinct.
    Type of Medium: Series available for loan
    Pages: iii, 21 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 250
    Language: English
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  • 85
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    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-249
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Analytical procedures. - Results and discussion. - Bubbles in ice. - Conclusions. - Literature cited.
    Description / Table of Contents: Application of the gas law to fourth-place density measurements of ice samples from two deep drill holes at Byrd Station and Little America V, Antarctica, shows that virtually all density increase beyond the pore close-off density (0.830 g/cm^3) can be attributed to compression of the entrapped bubbles of air. Data from Byrd Station also indicate that the lag between overburden pressure and bubble pressure, initially 4-5 kg/cm^2 at pore close-off, diminishes to less than 1.0 kg/cm^2 at about 200-m depth. By substituting the overburden pressure for the bubble pressure in the pressure-density relationship based on the gas law, ice densities below 200 m can be calculated more accurately than they can be measured per se on cores because of the relaxation that occurs in samples recovered from high confining pressures. This relaxation, resulting in a progressive increase in the bulk volume of the ice with time, is generally attributed to decompression of the entrapped air bubbles following removal of the ice from high confining pressures. However, calculations of the stress in ice due to bubble pressure, together with measurements of bubble sizes in cores from various depths at Byrd Station, both tend to indicate that there has'been negligible decompression of the inclosed bubbles. It is suggested that most of this relaxation may be due to the formation of microcracks in the ice. Anomalous bubble pressure-density relations at Little America V tend to confirm abundant stratigraphic evidence of the existence of considerable deformation in the upper part of the Ross Ice Shelf. Studies of crystal-bubble relations at Byrd Station revealed that the concentration of bubbles in ice remains remarkably constant at approximately 220 bubbles per cm^3. Bubbles and crystals were found to be present in approximately equal numbers at pore close-off at 64-m depth, at which level the average bubble diameter was 0.95 mm, decreasing to 0.49 mm at 116 m and to 0.33 mm at 279 m. Despite a tenfold increase in the size of crystals between 64 and 279 m, the bubbles showed no tendency to migrate to grain boundaries during recrystallization of the ice. The observation that most of the bubbles had assumed substantially spherical shapes by 120-m depth points to essentially hydrostatic conditions in the upper layers of the ice sheet at Byrd Station.
    Type of Medium: Series available for loan
    Pages: iv, 16 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 249
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  • 86
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    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
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    Call number: ZSP-202-248
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Analytical procedures. - Results and discussion. - Literature cited.
    Description / Table of Contents: Conductivity measurements have been made on snow and ice samples from pits and deep drillholes at a number of localities in Antarctica and Greenland. Conductivities of the order 1-2 [My]mho/cm only were recorded at the inland sites. Data from deep cores representing more than 1900 years of continuous snow accumulation at Byrd Station, Antarctica, and more than 400 years deposition at Inge Lehmann, Greenland, showed no significant variations of conductivity with time. Measurements of freshly precipitated snow from a single coastal location in McMurdo Sound, Antarctica, also yielded relatively low conductivities of the order 3-4 [My]mho/cm. The substantial increase observed in the conductivity of core samples from near the surface of the Ross Ice Shelf at Little America V can be attributed most probably to windborne salts of marine origin that had accumulated on the surface after the snow was deposited. A peak conductivity of 49 [My]mho/cm was recorded in snow estimated to have been deposited within 20 km of the seaward edge of the Ross Ice Shelf and the maritime effect could still be detected in samples deposited more than 40 km from the ice front. For samples deposited at distances of greater than 200 km from the edge of the Ross Ice Shelf conductivities never exceeded 2 [My]mho/cm. The very low conductivities observed in ice cores from near the bottom of the Ross Ice Shelf confirm earlier conclusions based on detailed petrographic studies oi the cores that the 258-m-thick ice shelf at Little America V is composed entirely of glacial ice.
    Type of Medium: Series available for loan
    Pages: iv, 8 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 248
    Language: English
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  • 87
    Call number: AWI PY-1892-13,2
    In: Die internationale Polarforschung 1882 - 1883
    Description / Table of Contents: Inhalt: 2. BAND: 1. ABTHEILUNG: POLARLICHT- UND SPECTRAL-BEOBACHTUNGEN, durchgeführt und bearbeitet von Linienschiffs-Lieutenant Adolf Bobrik von Boldva. - Einleitung. - Eintheilung des Beobachtungsmaterials. Beschreibung der aufgetretenen Formen und Definition der gebrauchten Ausdrücke. - Intensität des Lichtes. - Färbung der Polarlichterscheinungen. - Zugrichtung und Lichtbewegung. - Position und Höhe. Concentrationspunkt der Strahlen. - Polarlichter im Zusammenhange mit den magnetischen Störungen. - Abbildungen der Polarlichterscheinungen. - Polarlichter. - Tabellarische Zusammenstellungen. - Häufigkeit des Auftretens der verschiedenen Polarlichtformen in den einzelnen Richtungen ; Zugrichtung, Lichtbewegung und Intensität. - Höhe der Polarlichter über der Erdoberfläche ; Zusammenhang mit dem Wetter. - Die tägliche und jährliche Periode des Polarlichtes zu Jan Mayen. - Tabellen I-IX. - Spectralbeobachtungen und Farbe des Polarlichtes. - 2. ABTHEILUNG: MAGNETISCHE BEOBACHTUNGEN, bearbeitet von Linenschiffs-Lieutenant August Gratzl. - Einleitung. - Absolute Bestimmungen. - Declination. - Horizontal-Intensität. - Inclination. - Variationsapparate. - A. Die Wild-Edelmann'schen Apparate. - 1. Das Declinatorium. - 2. Das Bifilar-Magnetometer. - 3. Die Lloyd'sche Wage. - B. Die Lamont-Edelmann'schen Apparate. - 1. Das Unifilar. - 2. Das Unifilar mit Ablenkungsmagneten. - 3. Das Unifilar mit Eisenstäben. - Terminbeobachtungen. - Stündliche Beobachtungen. - Berechnung der Perioden. - Declination. - Horizontal-Intensität. - Vertical-Intensität. - Total-Intensität. - Inclination. - Störungen. - Normaltage. - Zusammenhang zwischen Polarlichtern und magnetischen Störungen. - Zusammenhang zwischen magnetischen Störungen und Sonnenflecken. - Gleichzeitige Änderung der verschiedenen Elemente bei Störungen. - Absolute Bestimmungen in der Umgegend der Station. - Schlusswort. - Tabellen. - Terminbeobachtungen: Termintage, Terminstunden. - Stündliche Beobachtungen der Declination. - Monatsstundenmittel der Declination. - Monatsstundenmittel der Inclination. - Monatsstundenmittel der Total-Intensität. - Stündliche Beobachtungen der Horizontal-Intensität. - Monatsstundenmittel der Horizontal-Intenstität. - Stündliche Beobachtungen der Vertical-Intensität. - Monatsstundenmittel der Vertical-Intensität. - Tagesmittel der Total-Intensität. - Tagesmittel der Inclination. - Zusammenstellung der Abweichungen der Declination. - Zusammenstellung der Abweichungen der Horizontal-Intensität. - Zusammenstellung der Abweichungen der Vertical-Intensität. - 3. BAND: Einleitung, von Dr. Ferndinand Fischer. - VI. THEIL: ZOOLOOGIE. - A. Foraminiferen, bearbeitet von Dr. Victor Uhlig. - B. Poriferen, Anthozoen, Ctenophoren und Würmer, bearbeitet von Dr. Emil von Marenzeller. - C. Polypomedusen, bearbeitet von Dr. Ludwig von Lorenz. - D. Echinodermen, bearbeitet von Dr. Ferdinand Fischer. - E. Crustaceen, Pycnogoniden und Arachnoiden, bearbeitet von Carl Koelbel. - F. Insecten, bearbeitet von Dr. Eduard Becher. - G. Mollusken, bearbeitet von Dr. Eduard Becher. - H. Bryozoen, bearbeitet von Dr. Ludwig von Lorenz. - I. Tunicaten, bearbeitet von Dr. Richard Freiherrn von Drasche. - K. Fische, bearbeitet von Dr. Franz Steindachner. - L. Vögel und Säugetiere, bearbeitet von Dr. F. Fischer und August von Pelzeln. - VII. THEIL: BOTANIK. - A. Flora der Insel Jan Mayen, bearbeitet von Dr. H. W. Reichardt. - B. Untersuchungen einiger Treibhölzer, ausgeführt von Josef Schneider. - VII. THEIL: MINERALOGIE. - Gesteine von Jan Mayen, bearbeitet von Dr. Fritz Berwerth.
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  • 88
    Call number: AWI PY-1895-13,1 ; AWI PY-1895-13,1(2. Ex.)
    In: Observations faites au Cap Thordsen, Spitzberg, par l'expédition suedoise
    Type of Medium: Monograph non-lending collection
    Pages: getr. Zählung : Abb., Kt.
    Note: Content: Introduction historique / par Nils Ekholm. - Observations astronomiques, géodésiques et marégraphiques / par Nils Ekholm. - Appendice: Reconnaissances géographiques / par H. Stjernspetz. - Observations météorologiques / par Nils Ekholm. - Magnétisme terrestre / par E. Solander.
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  • 89
    Call number: Q 699(2,1) / Regal 52
    In: Astronomische Beobachtungen aus der Königlichen Sternwarte zu Berlin
    Type of Medium: Monograph available for loan
    Pages: (28), 591 S.
    Series Statement: Astronomische Beobachtungen aus der Königlichen Sternwarte zu Berlin : 2. Serie 2, 1
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  • 90
    Call number: AWI PY-1893-13,1
    In: Report on the proceedings of the United States expedition to Lady Franklin Bay, Grinnell Land
    Description / Table of Contents: Contents: Report of the commanding officer. - Appendices. - 1. War Department order assigning Lieutenant Greely to command. - 2. War Department order organizing the expedition. - 3. Instructions from the Signal Office regarding the expedition. - 4. List of commissary subsistence stores, with remarks thereon. - 5. Records left at and taken from Southeast Cary Island, August, 1881. - 6. Lieutenant Kislingbury's report of trip to Life Boat Cove. - 7. Records taken from and left at Washington Irving Island, August, 1881. - 8. Records obtained at Discovery Harbor, August 1, 1881. - 9. Lieutenant Lockwood's report on Water-course Bay, August, 1881. - 10. Lieutenant Kislingsbury's request to be relieved, with Lieutenant Greely's indorsement. - 11. Orders No. 5, relieving Lieutenant Kislingsbury and ordering him to report to the Chief Signal Officer. - 12. Orders No. 6 amending Orders No. 5. - 13. Lieutenant Kislingsbury's request for modification of Orders No. 6. - 14. Orders No. 8 modifying Orders No. 6. - 15. Lieutenant Lockwood's report on exploration of St. Patrick Valley. - 16. Sergeant Brainard's report establishing Depot B near Cape Beechy. - 17. Sergeant Jewell's meteorological report in connection with trip establishing Depot B. - 18. Sergeant Gardiner's report of trip to Cape Murchison. - 19. Sergeant Linn's report on moving Depot A to Cape Murchison. - 20. Orders to Dr. Pavy for overland journey to Lincoln Bay. - 21. Report of Dr. Pavy on trip to Lincoln Bay. - 22. Report of Lieutenant Lockwood on journey to the Bellows. - 23. Orders to Dr. Pavy on exploring Archer Fiord. - 24. Report of Dr. Pavy on attempted trip down Archer Fiord. - 25. Report of Lieutenant Lockwood on sledge journey to Depot B near Cape Beechy. - 27. Orders to Dr. Pavy to proceed to Cape Joseph Henry. - 28. Report of Dr. Pavy on trip towards Cape Joseph Henry. - 29. Lieutenant Lockwood's report on St. Patrick Valley. - 30. Sergeant Rice's report on camp equipage. - 31. Lieutenant Lockwood's orders to attempt crossing of Robeson Channel. - 32. Lieutenant Lockwood's report on attempted crossing of Robeson Channel. - 33. Dr. Pavy's orders for journey to Wrangel Bay. - 34. Dr. Pavy's report on journey to Wrangel Bay. - 35. Dr. Pavy's supplementary report under Appendices 27 and 33. - 36. Lieutenant Lockwood's orders for preliminary journey to Cape Beechy. - 37. Lieutenant Lockwood's report on journey ordered in Appendix No. 36. - 38. Lieutenant Lockwood's orders for journey to Thank God Harbor. - 39. Lieutenant Lockwood's report on journey ordered in Appendix No. 38. - 40. English records obtained at Thank God Rarbor. - 41. Dr. Pavy's orders to carry provisions to Greenland coast. - 42. Dr. Pavy's report on journey ordered in Appendix No. 41. - 43. Sergeant Brainard's orders to move boat to Greenland coast. - 44. Sergeant Brainard's report on trip ordered in Appendix No. 43. - 45. Sergeant Jewell's report on trip to Lincoln Bay while supporting Dr. Pavy. - 46. Dr. Pavy's orders for journey northward over Polar Ocean. - 47. Dr. Pavy's report on journey ordered in Appendix No. 46. - 48. Sergeant Rice's report on detached trip from Lincoln Bay to Fort Conger and return. - 49. Private Long's report on trip into Archer Fiord. - 50. Sergeant Israel's report on trip into the Bellews. - 51. Lieutenant Lockwood's orders lo explore north coast of Greenland. - 52. Supplementary instructions for exploration of north coast of Greenland. - 53. Lieutenant Lockwood's report on exploration of north coast of Greenland. - 54. Report of Private Biederbick's trip into Black Rock Vale. - 55. Sergeant Linn's report of trip into Black Rock Vale. - 56. Lieutenant Lockwood's report of launch trip up Archer Fiord. - 57. Lieutenant Lockwood's report of launch trip up Chandler Fiord. - 58. Dr. Pavy's orders to proceed to Carl Ritter Bay. - 59. Sergeant Elison's report of trip to Carl Ritter Bay. - 6o. Sergeant Brainard's report of trip to Carl Ritter Bay. - 61. Orders establishing day of "Thanksgiving". - 62. Dr. Pavy's Ietter of March 8, 1883. - 63. Lieutenant Greely's answer to Dr. Pavy's Ietter of March 8, 1883. - 64. Lieutenant Lockwood's orders for preliminary journey northward, 1883. - 65. Lieutenant Lockwood's report on journey ordered in Appendix No. 64. - 66. Sergeant Jewell's report to Lieutenant Lockwood relative to journey ordered in Appendix No. 64. - 67. Orders to Lieutenant Lockwood for exploration of Greenland, 1883. - 68. Sergeant Rice's orders for journey to Thank God Harbor. - 69. Dr. Pavy's orders for journey, as surgeon, to Thank God Harbor. - 70. Lieutenant Lockwood's report on trip to North Greenland. - 71. Sergeant Jewell's report on tidal and meteorological observations made on trip to North Greenland. - 72. Sergeant Rice's report on trip to Thank God Harbor. - 73. Dr. Pavy's medical report on trip to Thank God Harbor. - 74. Orders for Sergeant Jewell for tidal observations at Cape Beechey. - 75. Report of Sergeant Jewell on tidal observations at Cape Beechey. - 76. Orders for Sergeant Gardiner for tidal Observations at Cape Baird. - 77. Orders for Sergeant Israel for astronomical Observations at Cape Baird. - 78. Report of Sergeant Israel on observations ordered in Appendix No. 77. - 79. Report of Sergeant Gardiner on tidal and ice observations at Cape Baird. - 80. Report of Sergeant Jewell on paleocrystic ice. - 81. Orders to Sergeant Jewell for tidal Observations at Cape Beechey. - 82. Report of Sergeant Jewell on tidal Observations at Cape Beechey. - 83. Sergeant Brainard's report on journey to Cape Cracroft. - 84. Sergeant Gardiner's report on journey to Cape Cracroft. - 85. Lieutenant Lockwood's orders to cross Grinnell Land. - 86. Lieutenant Lockwood's report on the crossing of Grinnell Land. - 87. Orders to Dr. Pavy relative to natural history data. - 88. Orders to Dr. Pavy relative to botanical specimens. - 89. Orders to Lieutenant Lockwood to relieve Dr. Pavy as naturalist. - 90. Lieutenant Lockwood's report on natural history specimens received from Dr. Pavy. - 91. Lieutenant Lockwood's Ietter and report on natural history specimens, June 30, 1883. - 92. Sergeant Brainard's report on Lieutenant Lockwood's trip towards the United States Mountain range. - 93. Orders to Lieutenant Lockwood to receive medical stores from Dr. Pavy. - 94 Letter of Dr. Pavy asking the detail of Steward Biederbick. - 95. Reply of Lieutenant Greely to Dr. Pavy's request for detail of Steward Biederbick. - 96. Letter of Dr. Pavy's, dated July 18, 1883. - 97.Answer to Ietter referred to in Appendix No. 96. - 98. Dr. Pavy's refusal to turn over his diary. - 99. Letter transmitting charges to Dr. Pavy. - 100. Letter limiting Dr. Pavy's bounds while in arrest. - 101 Order for the abandonment of station at Fort Conger. - 102. List of subsistence stores abandoned. - 103. Medical reports. - 104. Record left at Cape Baird. - 105. Records left in abandoned boats. - 106. Records found on Brevoort Island ( deposited by Lieutenant Garlington and Private Beebe). - 107. Plan of winter quarters, Camp Clay. - 108. Sergeant Frederick's report of November journey to Cape Isabella. - 109. Lieutenant Kislingsbury's letter, February 19, 1884. - 110. Private Long's journey into Hayes Sound. - 111. Sergeant Frederick's report of journey to Baird Inlet, April, 1884. - 112. Lieutenant Kislingsbury's letter, April 22, 1884. - 113. Letter of Dr. Pavy's, April 25, 1884. - 114. Letter of Dr. Pavy, April 27, 1884. - 115. Lieutenant Greely's certificate to Dr. Pavy. - 116. - General certificate to Dr. Pavy. - 117. Letter of Lieutenant Greely on Dr. Pavy. - 118. - Oder for Private Henry's execution. - 119. Report of Private Henry's execution. - 120. Letter of Secretary of War approving Lieutenant Greely's course regarding execution of Private Henry. - 121. List of deaths. - 122. Order relative to Private Henry, dated June 5, 1884. - 123. Lieutenant Lockwood's journal from August 3, 1883. - 124. Sergeant Brainard's journal from besetment. - 125. Portion of diary of Private Roderick R. Schneider, found on bank of Mississippi River, in Missouri, and correspondence relating thereto with Mr. J. A. Ockerson. - 126. Description of drift-wood. - 127. List of photographs and description of Eskimo relics in photographic plates. - 128 List of maps and charts. - Index to Vol. 1.
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    Pages: VIII, 545 : Taf., 1 Kt.
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  • 91
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    Call number: AWI PY-2895-13
    In: Trudy russkoj poljarnoj stancii na Novoj Zemle
    Type of Medium: Monograph non-lending collection
    Pages: XVII, 142 S. : graph. Darst., Ill.
    Note: Inhaltsverzeichnis: 1. THEIL. MAGNETISCHE BEOBACHTUNGEN. - Vorwort. - Liste des Commandos. - Einleitung. - 1. Astronomische Beobachtungen. - 2. Magnetische Beobachtungen. - 2.1 Absolute Bestimmungen. - Kleine Karmakul: magnetische Beobachtungen für 1882-1883. - Kleine Karmakul: absolute Bestimmungen. - Kleine Karmakul: Declination. - Kleine Karmakul: Horizontalintensität. - Kleine Karmakul: Inclination und Verticalintensität. - Kleine Karmakul: stündliche magnetische Beobachtungen. - Kleine Karmakul: Declination. - Kleine Karmakul: horizontale Componente der erdmagnetischen Kraft. - Kleine Karmakul: Verticale Componente der erdmagnetischen Kraft. - Kleine Karmakul: Resumé der magnetischen Beobachtungen für 1882-1883. - Kleine Karmakul: Stundenmittel. - Kleine Karmakul: Terminbeobachtungen für 1882 - 1883. - Kleine Karmakul: Declination. - Kleine Karmakul: horizontale Componente der erdmagnetischen Kraft. - Kleine Karmakul: Verticale Componente der erdmagnetischen Kraft. - 2. THEIL. METEOROLOGISCHE BEOBACHTUNGEN. - Einleitung. - Kleine Karmakul: stündliche meteorologische Beobachtungen. - Kleine Karmakul: Luftdruck. - Kleine Karmakul: Temperatur der Luft. - Kleine Karmakul: Feuchtigkeit der Luft. - Kleine Karmakul: Richtung und Geschwindigkeit des Windes. - Kleine Karmakul: Menge und Form der Wolken, Niederschläge u.s.w. - Kleine Karmakul: Temperatur auf der Oberfläche des Bodens. - Kleine Karmakul: Bodentemperatur in 0,4 m Tiefe. - Kleine Karmakul: Bodentemperatur in 0,8 u. 1.6 m Tiefe. - Kleine Karmakul: Resumé der meteorologischen Beobachtungen für 1882 - 1883. - Kleine Karmakul: Stundenmittel. - Kleine Karmakul: Tagesmittel. - Kleine Karmakul: Rosen. - Kleine Karmakul: Monatsmittel. - Anhang No. 1: Pegelbeobachtungen. - Anhang No. 2: Längen- und Breitenbestimmung. , In russ. und dt. Sprache mit z. T. kyrill. Schr.
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  • 92
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    Hanover, N.H. : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-349
    In: Research report / Cold Regions Research and Engineering Laboratory, 349
    Description / Table of Contents: CONTENTS: Abstract. - Preface. - Introduction. - Test locations. - Post Pond. - Mascoma Lake. - Winter freeze-up. - Ice cover properties. - Stratigraphy. - Microstructure. - Porosity. - Impurity content. - Flexural strength. - Test sites. - Beam test procedure. - Beam dimensions. - Beam temperatures. - Beam strengths. - Results. - Post Pond, Site PB, 12 February 1974. - Post Pond, Site PC, 21 February 1974. - Mascoma Lake, Site MD, 25 February 1974. - Mascoma Lake, Site MD, 26 February 1974. - Mascoma Lake, Site MD, 1 March 1974. - Post Pond, Site PA, 4 March 1974. - Post Pond, Site PA, 7 March 1974. - Post Pond, Site PA, 8 March 1974. - Post Pond, Site PB, 12 March 1974. - Post Pond, Midway between Sites PB and PC, 15 March 1974. - Post Pond, Midway between Sites PA and PB, 26 March 1974. - Post Pond, Midway between Sites PA and PB, 29 March 1974. - Post Pond, Midway between Sites PA and PB, 3 April 1974. - Conclusions. - Literature cited.
    Description / Table of Contents: In-place cantilever beam tests on Post Pond and Mascoma Lake ice yielded a maximum flexural strength of 7.1 kg/cm^2. The minimum strength, unrelated to failure along pre-existing cracks in the ice, was 2.9 kg/cm^2. The majority of tests were performed in the push-down mode after it was discovered that beams tested in the pull-up mode, which places the bottom surface in tension, frequently broke prematurely along cracks in the bottom of the ice. Premature failures of this kind usually occurred at stresses of 2-3 kg/cm^2. Data further demonstrate that the intrinsic strength of lake ice decreases significantly as the surface air temperature goes to 0°C. Ice that has just become isothermal, but has not yet begun to candle, has a strength of about 4 kg/cm^2; ice that has been subjected to prolonged periods of above-freezing air temperatures generally fails at about 3 kg/cm^2. Tests also show that cold unrecrystallized snow-ice is as strong as the underlying lake ice. Tests of the effect of crystalline structure indicate that ice composed of crystals with their c-axes horizontal is measurably stronger than ice in which the crystals are oriented with their c-axes vertical.
    Type of Medium: Series available for loan
    Pages: v, 28 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 349
    Language: English
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  • 93
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    Hanover, NH : Corps of Engineers, U.S. Army Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-261
    In: Research report
    Description / Table of Contents: This paper considers a load moving with a constant velocity across an ice sheet that is floating on water. The ice sheet is assumed to be an isotropic, elastic, thin plate extending to infinity. The water is assumed to be inviscous, incompressible, and of a constant depth. The dynamic equations describing this ice-water system are solved for the steady state solution. Both a concentrated load and a uniform load distributed over a circular area are considered. The velocity which causes resonance is determined. The deflection and stress directly under the load are numerically evaluated.
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    Pages: ii, 13 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 261
    Language: English
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  • 94
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    Hanover, NH : Corps of Engineers, U.S. Army, Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-259
    In: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command, 259
    Description / Table of Contents: CONTENTS: Preface. - Introduction. - Previous work. - Study area. - Field procedures. - Results and discussion. - Conclusions. - Literature cited. - Abstract.
    Description / Table of Contents: A modern ice-push ridge on the northwest shore of Gardner Lake in southeastern Connecticut is 0.6 - 1.2 m high and 1.2 - 3.1 m wide. In February and March 1967, the positions of survey stakes placed on the lake ice were measured periodically. During the same period, air and ice temperature and solar radiation intensity were also recorded. Analysis of the data supports the hypothesis that thermal expansion of the lake ice rather than wind action, was the principal cause of ice push. An ice temperature change of approximately 1°C/hr increase for 6 hr was sufficient to induce ice thrust. In a 30-day period, the average net shoreward movement of the surveyed area of the ice surface was 1.0 m. During the 1966-67 winter, approximately 14 m^3 of beach material was reworked and deposited, forming a discontinuous ice-push ridge along 260 m of shoreline.
    Type of Medium: Series available for loan
    Pages: iii, 15 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 259
    Language: English
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  • 95
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    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
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    Call number: ZSP-202-252
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Theory. - Discussion. - Conclusion. - Literature cited.
    Description / Table of Contents: A diffusion equation is obtained that describes the mechanical dispersion of a dilute mixture of solid particles within an ice matrix that is undergoing deformation. It is shown that within the limits of time intervals and strain rates appropriate to the movement of glaciers and ice sheets the dispersal distance usually is no larger than a distance about one order of magnitude greater than the size of the particles themselves.
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    Pages: iv, 6 Seiten , Illistrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 252
    Language: English
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  • 96
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    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
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    Call number: ZSP-202-253
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Theoretical considerations. - Method of canopy evaluation. - Application to forest problems. - Forest blowdown. - Radioactivity gradient. - Phenology. - Forest types and structure. - Distribution of leaves and canopy gaps. - Light quality. - Discussion and summary. - Literature cited.
    Description / Table of Contents: A technique for evaluating forest canopies was developed based on the use of a divergent lens system to obtain hemispherical photographs of tree crowns. The photography was processed from 35 mm film and enlarged as a silhouette, and the light transmission was measured with a specially fabricated macrodensitometer. It is concluded that the amount of forest canopy can be expressed as canopy closure index (CCI) at a precision of approximately 5%. It is shown by application to a variety of problems in diverse geographical areas that this technique can be used for measuring both temporal and spatial changes in the canopy, for estimating the shade light climate, and for specifying the probability of target detection through a canopy. Data are presented to analyze changes caused by explosions, radioactivity, growing season, and vegetation types. The geometry of gaps in tree crowns is discussed and the nature of shade light quality under forests is illustrated.
    Type of Medium: Series available for loan
    Pages: v, 20 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 253
    Language: English
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  • 97
    Call number: AWI PY-1895-13,2 ; AWI PY-1895-13,2(2. Ex.)
    In: Observations faites au Cap Thordsen, Spitzberg, par l'expédition suedoise
    Description / Table of Contents: Content: Aurores boreales / par Carlheim-Gyllenskiöld. - Électricité atmosphérique / par S. A. Andrée. - Phénomènes optiques de l'atmosphère, avec quelques remarques sur les Étoiles filantes, le spectre des Copépodes, l'accroissement des brins d'orge / par Carlheim-Gyllenskiöld. - Recherches sur le prétendu changement de la couleur de la peau après un hivernage dans les régions polaires / exécutées par R. Gyllencreutz, communiquées par Frithiof Holmgren.
    Type of Medium: Monograph non-lending collection
    Pages: getr. Zählung : Abb., Kt.
    Location: AWI Archive
    Location: AWI Archive
    Branch Library: AWI Library
    Branch Library: AWI Library
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  • 98
    Monograph non-lending collection
    Monograph non-lending collection
    Associated volumes
    Call number: AWI PY-1788-13
    Type of Medium: Monograph non-lending collection
    Pages: 237 S., XLVII Bl. : graph. Darst.
    Note: Upsala, Univ., Diss., 1888 , Table des Matières: Introduction. - 1. Déterminations de l'influence de la température sur les aimants et les déflecteurs. - 2. Constantes d'induction des aimants. - 3. Déterminations du moment d'inertie K de l'aimant II d'Edelmann. - 4. Déterminations de la constante k (Notation de Lamont) de l'aimant II d'Edelmann. - 5. Détermination comparative des constantes. - 6. Installation des instruments de variations et détermination de leurs constantes. - 7. Déterminations absolues de la déclinaison faites dans le cabinet magnétique en vue de la détermination du point zéro de l'appareil de variations. - 8. Déterminations de la composante horizontale du magnétisme terrestre effectuées dans le cabinet magnétique de l'observatoire du Cap Thordsen. - 9. Déterminations de l'inclinaison exécutées dans le cabinet magnétique. - 10. Déterminations des constantes pour les déflecteurs A et B du théodolite de voyage de Lamont. - 11. Déterminations magnétiques pendant les excursions et dans les environs du cabinet magnétique. - 12. Lecture des instruments de variations et réduction des lectures en mesures absolues. - Remarques. - 1. Remarques aux lectures horaires. - 2. Remarques aux lectures de cinq minutes en cinq minutes aux jours termes. - 3. Remarques aux lectures de 20 seconds en 20 secondes. - 13. Tableaux des Observations. - 14. Variation diurne réguliere de la Déclinaison et de la composante horizontale. - 15. Tableaux des différences de la déclinaison et de la composante horizontale; perturbations dans ces éléments. - 16. Variation diurne de la composante verticale.
    Location: AWI Archive
    Branch Library: AWI Library
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  • 99
    Monograph available for loan
    Monograph available for loan
    B.-Friedenau : Askania-Werke
    Call number: M 07.0066 Regal 12
    Type of Medium: Monograph available for loan
    Pages: 32 S. , gr. 8 [Umschlagt.]
    Location: Magazine - must be ordered
    Branch Library: GFZ Library
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  • 100
    Series available for loan
    Series available for loan
    Warszawa : Warsaw Univ. of Technology, Inst. of Geodesy and Geodetic Astronomy
    Associated volumes
    Call number: S 94.0254(80) / Regal 35
    In: Reports on geodesy
    Type of Medium: Series available for loan
    Pages: 647 S.
    ISBN: 8385287795
    Series Statement: Reports on geodesy 80 = 2006,5
    Classification:
    Geodynamics
    Location: Magazine - must be ordered
    Branch Library: GFZ Library
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