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  • 1995-1999  (220)
  • 1980-1984  (68)
  • 1935-1939  (2)
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  • 1
    Monograph available for loan
    Monograph available for loan
    London ; New York : Taylor & Francis
    Call number: PIK B 160-03-0320
    Type of Medium: Monograph available for loan
    Pages: 256 p.
    Edition: 1. ed.
    ISBN: 0415192153
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    New York [u.a.] : Wiley
    Call number: AWI G7-93-0181/1 ; AWI G7-93-0181/2
    Description / Table of Contents: Contents: Chapter 1 Late Weichselian lce Sheets in Eurasia and Greenland / Bjöm G. Andersen. - NORTHERN EUROPE. - Holland. - Germany. - Denmark. - Sweden. - Finland. - Poland. - Western USSR (including Baltic SSR). - Northwestern USSR. - Norway. - North Sea. - British Isles. - lceland. - SOUTHERN EUROPE. - BARENTS SEA AND ARCTIC ISLANDS. - ASIA. - GREENLAND. - REFERENCES CITED. - Chapter 2 Late Wisconsin Ice Sheets of North America / Paul A. Mayewski, George H. Denton, Terence J. Hughes. - INTRODUCTION. - LAURENTIDE ICE SHEET. - Eastern Sector. - Southern Sector. - Western Sector. - Northern Sector. - Northeastern Sector. - Interior Sector. - QUEEN ELIZABETH ISLANDS. - Late Wisconsin Maximum. - Late Wisconsin Recession. - CORDILLERAN ICE SHEET. - Late Wisconsin Maximum. - Late Wisconsin Recession. - NORTH AMERICAN ICE SHEETS: AN OVERVIEW . - Maximum and Minimum. - Reconstructions. - Fundamental Questions About Late Wisconsin Deglaciation. - Glaciological Speculations. - REFERENCES CITED. - APPENDIX. - Chapter 3 Late Wisconsin-Weichselian Mountain Glaciers and Small Ice Caps / John T. Hollin, David H. Schiling. - INTRODUCTION. - ALASKA. - WESTERN UNITED STATES. - MEXICO AND CENTRAL AMERICA. - SOUTH AMERICA. - Venezuela. - Colombia. - Ecuador. - Peru. - Bolivia. - Chile and Argentina to Lat 36°30'S. - Chile and Argentina South of Lat 36°30'S. - Islas Juan Fernandez. - Falkland Islands (Islas Malvinas). - Brazil. - Areas and Volumes. - NEWZEALAND. - AUSTRALIA, NEW GUINEA, AND SABAH. - The Australian Mainland. - Tasmania. - New Guinea and Sabah. - Conclusions. - AFRICA. - Northwest Africa and Atlantic Islands. - Mountains in Ethiopia. - Mountains Surrounding Lake Victoria. - South and West Africa. - SUBANTARCTIC ISLANDS. - CONCLUSIONS. - REFERENCES CITED. - Chapter 4 Numerical Reconstruction of Valley Glaciers and Small Ice Caps / David H. Schilling, John T. Hollin. - INTRODUCTION. - VALLEY GLACIERS AND PERFECT PLASTICITY. - The Iterative Scheme. - The Shape Factor. - Choice of the Yield Stress. - Choice of Step Length, [Delta x]. - The First Step and the Snout. - Steep and Mountainous Areas. - The VALLEY Program. - ICE CAPS, WITH SLIDING AND ABLATION. - Perfect Plasticity. - Law of Sliding and Iterative Scheme. - The ABLATE Program. - Various Models and the Flow Law. - An Application of the ABLATE Program. - Some Remaining Problems. - CONCLUSIONS. - REFERENCES CITED. - Chapter 5 Numerical Reconstruction of Paleo-Ice Sheets / Terence J. Hughes. - ICE-BED COUPLING AND SUBGLACIAL HYDROLOGY. - SUBGLACIAL HYDROLOGY AND EROSION-DEPOSITION PROCESSES. - TOPOGRAPHIC CRITERIA FOR RECONSTRUCTING FORMER ICE SHEETS. - Subglacial Landscapes. - Ice Domes. - Ice Saddles. - Melting Zone. - Equilibrium Zone. - Freezing Zone. - Ice Streams. - BASIC EQUATIONS FOR STEADY-STATE CREEP IN ICE SHEETS. - BASAL SHEAR STRESS AND TWO-DIMENSIONAL LAMINAR FLOW. - BASAL SHEAR STRESS AND BASAL SLIDING. - BASAL SHEAR STRESS AND CONSTRUCTING ICE-SHEET PROFILES. - BASAL SHEAR STRESS FOR FROZEN AND MELTED BEDS. - BASAL SHEAR STRESS FOR FREEZING AND MELTING BEDS. - BASAL SHEAR STRESS FOR ICE STREAMS AND ICE LOBES. - BASAL SHEAR STRESS FOR ICE DIVIDES. - EVALUATING TERMS IN THE FLOW AND SLIDING LAWS FOR GLACIAL ICE. - RADIAL FLOW AND SNOW ACCUMULATION FOR ICE DOMES. - LATERAL SHEAR AND DOWNDRAW FOR ICE STREAMS. - ISOSTATIC ADJUSTMENTS BENEATH ICE SHEETS. - SUMMARY. - REFERENCES CITED. - Chapter 6 The Last Great Ice Sheets: A Global View / Terence J. Hughes, George H. Denton, Björn G. Andersen, David H. Schilling, James L. Fastook, Craig S. Lingle. - AREAL EXTENT OF LATE WISCONSIN-WEICHSELIAN ICE SHEETS. - North America. - Greenland. - Eurasia. - Antarctica. - Minimum and Maximum. - Reconstructions of Late Wisconsin-Weichselian Ice Extent. - VERTICAL EXTENT OF LATE WISCONSIN-WEICHSELIAN ICE SHEETS. - The Critical Problem of Marine Ice Sheets. - Flowline Profiles for Variable Bed Topography. - Flowline Profiles for Variable Isostatic Compensation. - Flowline Profiles for Variable Basal Shear Stress. - Flowline Profiles for Present-day Ice Sheets. - Flowline Profiles for Late Wisconsin-Weichselian Ice Sheets. - Isostatic Conditions for Late Wisconsin-Weichselian Ice Sheets. - Basal Conditions for Late Wisconsin-Weichselian Ice Sheets. - Elevations and Volumes of Late Wisconsin-Weichselian Ice Sheets. - DISCUSSION. - REFERENCES CITED. - Chapter 7 History of the Marine Ice Sheet In West Antarctica During the Last Glaciation: A Working Hypothesis / Minze Stuiver, George H. Denton, Terence J. Hughes, James L. Fastook. - INTRODUCTION . - McMURDO SOUND AREA. - Ross Sea Drift: Description. - Ross Sea Drift: Interpretation. - Radiometric Dates and Ross Sea Drift. - Older Drift: Description and Interpretation. - Discussion. - TERRA NOVA BAY. - BEAUFORT AND FRANKLIN ISLANDS. - GLACIAL-MARINE SEDIMENTS IN THE ROSS SEA. - RECONSTRUCTION OF LATE WISCONSIN ANTARCTIC ICE SHEET. - Geologic Background. - Glaciological Background: Steady-State Model. - Conclusions. - DISINTEGRATION OF MARINE ICE SHEET IN WEST ANTARCTICA. - Disintegration Model. - Disintegration of Ice Shelves. - Late Wisconsin-Holocene Disintegration. - Disintegration during Super Interglacials. - SUMMARY. - REFERENCES CITED. - Chapter 8 The Arctic Ice Sheet: An Outrageous Hypothesis / George H. Denton, T erence J. Hughes. - ICE-SHELF ORIGIN OF NORTHERN HEMISPHERE ICE DOMES. - Growth Rates of Arctic Ice Domes. - Sites for lnitiating Arctic Ice Domes. - Thickening Rates of Arctic Sea Ice. - Sites for Grounding Arctic Sea Ice. - Forming Arctic Ice Shelves on Deep Oceans. - Assessing the lce-Shelf Hypothesis for Forming Marine Ice Domes. - LA TE WISCONSIN-WEICHSELIAN ARCTIC ICE SHEET. - Ice Domes. - Ice Streams. - Ice Shelves. - DISINTEGRATION OF LATE WISCONSIN-WEICHSELIAN ARCTIC ICE SHEET. - Initiation of Late Wisconsin-Weichselian Glacial Surges. - Maintenance of Late Wisconsin-Weichselian Glacial Surges. - Environmental Impact of Late Wisconsin-Weichselian Glacial Surges. - CONCLUSIONS. - REFERENCES CITED. - INDEX.
    Type of Medium: Monograph available for loan
    Pages: XVIII, 484 S. : Ill., Kt. ; 27 Kt.-Beil.
    ISBN: 0471060062
    Series Statement: A Wiley interscience publication
    Location: AWI Reading room
    Location: AWI Reading room
    Branch Library: AWI Library
    Branch Library: AWI Library
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  • 3
    Call number: MOP Per 701/B(NF, 74, 1-12)
    In: Meteorologische Abhandlungen
    Type of Medium: Monograph available for loan
    Pages: Getr. Zählung
    Series Statement: Meteorologische Abhandlungen : Serie B, Grundlagenmaterial N. F., 74, 1-12
    Location: MOP - must be ordered
    Branch Library: GFZ Library
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  • 4
    Electronic Resource
    Electronic Resource
    [S.l.] : American Institute of Physics (AIP)
    Physics of Plasmas 3 (1996), S. 3861-3863 
    ISSN: 1089-7674
    Source: AIP Digital Archive
    Topics: Physics
    Notes: Low-frequency magnetohydrodynamic equations including the effects of finite ion Larmor radius are derived. These equations contain all the physical terms necessary to describe kinetic Alfvén waves. Among other applications, these waves are used to interpret ultra-low-frequency wave phenomena in the Earth's magnetosphere. The finite ion Larmor radius effects are usually disregarded; however, under magnetospheric conditions, the ion temperature cannot be considered negligible since Ti≥Te. The finite ion gyroradius is accounted for by the ion stress tensor calculated in this Brief Communication. The nonlinear one-fluid system of equations is shown to adequately describe linear kinetic Alfvén waves in a low-β(β(very-much-less-than)1) homogeneous plasma. It is demonstrated that energy of the plasma system is conserved. © 1996 American Institute of Physics.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Woodbury, NY : American Institute of Physics (AIP)
    Applied Physics Letters 68 (1996), S. 3386-3388 
    ISSN: 1077-3118
    Source: AIP Digital Archive
    Topics: Physics
    Notes: In situ Fourier transform infrared spectroscopy (FTIR)/attenuated total reflection (ATR) was used to study the deposition of plasma polymerized methyl methacrylate (PPMMA) film. Real time absorption spectra of PPMMA films were obtained at a time resolution of 20–30 s which is mostly limited by the low optical throughput and low signal-to-noise ratio. Postplasma dynamics observed in the system demonstrate the need for an in situ and real time film diagnostic technique. This letter reports the use of this diagnostic on plasma deposited polymers. © 1996 American Institute of Physics.
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    College Park, Md. : American Institute of Physics (AIP)
    The Journal of Chemical Physics 104 (1996), S. 805-811 
    ISSN: 1089-7690
    Source: AIP Digital Archive
    Topics: Physics , Chemistry and Pharmacology
    Notes: We present a comparative study on the ultrafast nonlinear optical response of a novel conjugated zinc porphyrin system. The linear optical absorption spectra of these molecules all show the Q-band and B-band transitions of the basic porphyrin unit. We have taken spectrally resolved ultrafast pump–probe measurements on monomer, dimer, and polymer solutions, which allows us to compare their excited state dynamics and relate these to their linear optical absorption. The spectra show several common features, but these features have markedly different decay dynamics. The bleaching is preferential in the Q band for the polymer and the B band for the monomer. The polymer Q-band bleaching shows a two-component decay, of approximately 700 fs and 170±50 ps time constants in a biexponential fit, which we attribute to both exciton–exciton annihilation and exciton diffusion to recombination centers on the polymer chain. The Q band of the dimer also has a two-component decay with 13±5 and 1250±70 ps time constants which we attribute to rotational diffusion of the excited molecule in solution, and decay to the ground state, respectively. The B-band bleaching in the monomer is long lived and has a decay constant of approximately 3.5±0.5 ns; from the absorption recovery of the B band we estimate a triplet yield of 0.8. All molecules exhibit broad π*−π* absorptions in the visible spectral region (between the Q band and the B band). In particular, we show that the monomer has potential as a broadband optical limiter in the visible region from 455 (2.72 eV) to 620 nm (2.00 eV); we estimate that its excited state absorption cross section is 8.5 times that of its ground state cross section at 532 nm (2.33 eV). There is also clear evidence of triplet transitions in the dimer and monomer; the triplet absorption feature ranging from 940 (1.32 eV) to 1000 nm (1.24 eV) rises 10 ps after excitation in the dimer which suggests a short intersystem-crossing time. © 1996 American Institute of Physics.
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Oxford, UK and Boston, USA : Blackwell Publishers Ltd
    Creativity and innovation management 7 (1998), S. 0 
    ISSN: 1467-8691
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Economics
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Woodbury, NY : American Institute of Physics (AIP)
    Applied Physics Letters 66 (1995), S. 2072-2073 
    ISSN: 1077-3118
    Source: AIP Digital Archive
    Topics: Physics
    Notes: In this letter, a method is outlined and results presented for an x-ray lithography micromachining process that offers a greatly improved sensitivity over the LIGA process. This process is based on photosensitive polyimide (PPI), which is a commercial photoresist typically used as a passivation layer or dielectric material in the semiconductor industry. The main benefit of this process is its high sensitivity, which is approximately two orders of magnitude greater than that of the PMMA used in the LIGA process. Using a synchrotron radiation x-ray source, we have achieved resist patterns over 1000 μm thick. The capability has also been demonstrated for aspect ratios over 10, as well as the ability to print linewidths down to 0.5 μm. © 1995 American Institute of Physics.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Woodbury, NY : American Institute of Physics (AIP)
    Applied Physics Letters 67 (1995), S. 238-240 
    ISSN: 1077-3118
    Source: AIP Digital Archive
    Topics: Physics
    Notes: We report measurements of the polarization and time-averaged intensity of four-wave mixing signals from GaAs quantum wells as functions of the pump beam polarizations, laser photon energy, and optical injection density, the latter covering a range of higher levels than has previously been reported. Excitation of heavy-hole excitons produced a sin2 variation of the signal intensity as the pump beam polarizations changed from parallel to perpendicular, while injection of light-hole excitons led to an approximately cos2 dependence. The tuning dependence of the heavy-hole-exciton signal revealed a low-energy signal which is attributed to biexcitons. The dominance of this signal for perpendicular polarization causes the observed sin2 variation of the heavy-hole-exciton signal. © 1995 American Institute of Physics.
    Type of Medium: Electronic Resource
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  • 10
    ISSN: 1520-6882
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
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