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  • 1
    Monograph available for loan
    Monograph available for loan
    Dordrecht [u.a.] : Kluwer
    Associated volumes
    Call number: AWI A2-07-0063
    In: Atmospheric and oceanographic sciences library, 26
    Description / Table of Contents: This monograph presents a comprehensive synthesis of our current state of knowledge concerning the climate of the Arctic, using the latest meteorological data. All meteorological elements are described in detail for the first time and an up-to-date review of the available literature for each element is given. Climatic regions are distinguished and described. The monograph also provides an account of the present state of research on climate change and variability in the Arctic for three time scales: the Holocene, the last Millennium, and the 20th century. The book concludes with a presentation of the scenarios of the Arctic climate in the 21st century. This monograph is intended for all those with a general interest in the fields of meteorology, climatology, and with a knowledge of the application of statistics in these areas.
    Type of Medium: Monograph available for loan
    Pages: XI, 270 Seiten , Illustrationen
    ISBN: 1402011342
    Series Statement: Atmospheric and oceanographic sciences library 26
    Language: English
    Note: CONTENTS Preface Acknowledgements 1. Introduction 1.1 Boundaries of the Arctic 1.2 Main Geographical Factors Shaping the Climate 2. Atmospheric Circulation 2.1 Development of Views on Atmospheric Circulation in the Arctic 2.2 Large-scale Atmospheric Circulation 2.3 Synoptic-scale Circulation 2.4 Winds 2.5 Local Circulation and Mesoscale Disturbances 3. Radiation Conditions 3.1 Sunshine Duration 3.2 Global Solar Radiation 3.3 Short-wave Net Radiation 3.4 Long-wave Net Radiation 3.5 Net Radiation and Other Elements of the Heat Balance 4. Air Temperature 4.1 Mean Monthly, Seasonal, and Annual Air Temperature 4.2 Mean and Absolute Extreme Air Temperatures 4.3 Temperature Inversions 5. Cloudiness 5.1 The Annual Cycle 5.2 Spatial Patterns 5.3 Fog 6. Air Humidity 6.1 Water Vapour Pressure 6.2 Relative Humidity 7. Atmospheric Precipitation and Snow Cover 7.1 Atmospheric Precipitation 7.2 Number of Days with Precipitation 7.3 Snow Cover 8. Air Pollution 9. Climatic Regions 9.1 The Atlantic Region 9.2 The Siberian Region 9.3 The Pacific Region 9.4 The Canadian Region 9.5 The Baffin Bay Region 9.6 The Greenland Region 9.7 The Interior Arctic Region 10. Climatic Change and Variability in the Holocene 10.1 Period 10-11 ka-l ka BP 10.2 Period 1 ka-O.l ka BP 10.3 Period 0.1 ka-Present 11. Scenarios of the Arctic Climate in the 21st Century 11.1 Model Simulations of the Present-day Arctic Climate 11.2 Scenarios of the Arctic Climate in the 21st Century References Copyright Acknowledgements Index
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 2
    Call number: AWI A4-15-0009
    Type of Medium: Monograph available for loan
    Pages: 174 S. : Ill., graph. Darst., Kt.
    ISBN: 9788389743060
    Language: English
    Note: Contents: Preface. - 1. Introduction. - 1.1. Research purpose. - 1.2. Research area and methodology. - 2. Atmospheric circulation and dynamic conditions. - 2.1. Atmospheric circulation. - 2.2. Atmospheric pressure. - 2.3. Wind. - 3. Radiation conditions. - 3.1. Cloud cover. - 3.2. Sunshine duration. - 3.3. Solar radiation. - 4. Thermal conditions. - 4.1. Ground temperature. - 4.2. Air temperature. - 5. Higric conditions. - 5.1. Relative air humidity. - 5.2. Precipitation. - 6. The influence of atmospheric circulation on temperature and humidity conditions. - 6.1. The influence of atmospheric circulation on temperature conditions. - 6.2. The influence of atmospheric circulation on humidity conditions. - 7. Comparison of meteorological conditions in the area of Forlandsundet in the summer seasons of 2010-2011 with meteorological conditions in the years of 1975-2011. - 7.1. Introduction. - 7.2. Kaffiøyra. - 7.3. Waldemar Glacier. - Appendixes.
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 3
    Call number: 12/M 10.0110
    Description / Table of Contents: Contents: Part 1 The European Backgroun - 1.1 Climate Change in Poland in the Past Centuries and its Relationship to European Climate: Evidence From Reconstructions and Coupled Climate Models.- 1. 2 Historical Climate in Central Europe During the Last 500 Years.- 1.3 Climatic Variations in the East European Plain During the Last Millennium: state-of-the-art.- 1.4 The Climate of Europe in Recent Centuries in the Context of the Climate of Mid to High Latitude Northern Hemisphere from Borehole Temperature Logs.- Part 2 The Climate of Poland in Recent Centuries: A Synthesis of Current Knowledge .-2.1 Instrumental Observations -2.2 Documentary Evidence.- 2.3 Dendrochronological Data.- 2.4 Geophysical Data .- 2.5 Summary and Concluding Remarks.- Part 3 The Climate of Poland and Europe in Recent Centuries: New Findings Results.- 3.1 Long-term Changes of Bioclimatic Conditions in Cracow (Poland).- 3.2 Climate Warming in the Czech Republic: Evidence Stored in Shallow Subsurface .- 3.3 History of the Gdansk Pre-instrumental and Instrumental Record of Meteorological Observations and Analysis of Selected Air Pressure Observations..- 3.4 A Composite Reconstruction of the Russian Arctic Climate Back to A.D. 1435.- 3.5 Growth/Climate Relationships in Tree-ring Widths of Picea abies in Lithuania and Poland.- 3.6 Multi-annual Variability of Cloudiness and Sunshine Duration in Cracow Between 1826 and 2005.- 3.7 Changes in Sea Surface Temperature of the South Baltic Sea (1854-2005).- 3.8 Ground Surface Temperature Histories Reconstructed from Boreholes in Poland: Implications for Spatial Variability.- 3.9 Precipitation Extremes and Disastrous Floods in Central Europe in July 1897.- 3.10 Summer Temperatures in the Tatra Mountains during the Maunder Minimum (1645-1715).- 3.11 Seasonal Differentiation of Maximum and Minimum Air Temperature in Cracow and Prague in the Period 1836-2007.- 3.12 Climate Changes in the Central and North-eastern Parts of the Polish-Lithuanian Commonwealth from 1656 to 1685.- 3.13 The Climate of Polish Lands as Viewed by Chroniclers, Writers and Scientists.- 3.14 Observations and Measurements of Precipitation in the Polish Province of Galicia in the Nineteenth Century.- 3.15 Variability of the European Climate on the Basis of Differentiation of Indicators of Continentalism.- 3.16 The First One Hundred Years (1791-1890) of the Wroclaw Air Temperature.
    Type of Medium: Monograph available for loan
    Pages: XVIII, 535 S. , Ill., graph. Darst., Kt.
    ISBN: 9789048131662
    Classification:
    Meteorology and Climatology
    Location: Reading room
    Branch Library: GFZ Library
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  • 4
    Call number: AWI A3-03-0009 ; M 05.0396
    In: Atmospheric and oceanographic sciences library
    Description / Table of Contents: Contents: Data and Methods. Variability in Atmospheric Circulation in the Arctic between 1939 and 1990. Variability of Air Temperature. Variability of Atmospheric Precipitation. Scenarios of Thermal-Precipitation Conditions in a Warmer World.
    Type of Medium: Monograph available for loan
    Pages: xv, 330 S.
    ISBN: 1402009526
    Series Statement: Atmospheric and oceanographic sciences library 25
    Uniform Title: Zmienno´s´c temperatury i opadów atmosferycznych w okresie obserwacji instrumentalnych w Arktyce
    Classification:
    Meteorology and Climatology
    Language: English
    Location: Upper compact magazine
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    Branch Library: GFZ Library
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  • 5
    Publication Date: 2020-04-01
    Description: The history of drought occurrence in Poland in the last millennium is poorly known. To improve this knowledge we have conducted a comprehensive analysis using both proxy data (documentary and dendrochronological) and instrumental measurements of precipitation. The paper presents the main features of droughts in Poland in recent centuries, including their frequency of occurrence, coverage, duration, and intensity. The reconstructions of droughts based on all the mentioned sources of data covered the period 996–2015. Examples of megadroughts were also chosen using documentary evidence, and some of them were described. Various documentary sources have been used to identify droughts in the area of Poland in the period 1451–1800 and to estimate their intensity, spatial coverage, and duration. Twenty-two local chronologies of trees (pine, oak, and fir) from Poland were taken into account for detecting negative pointer years (exceptionally narrow rings). The delimitation of droughts based on instrumental data (eight long-term precipitation series) was conducted using two independent approaches (Standard Precipitation Index, SPI, calculated for 1-, 3-, and 24-month timescales, and a new method proposed by authors). For delimitation of droughts (dry months), the criteria used were those proposed by McKee et al. (1993) and modified for the climate conditions of Poland by Łabędzki (2007). More than 100 droughts were found in documentary sources in the period 1451–1800, including 17 megadroughts. A greater than average number of droughts were observed in the second halves of the 17th century and the 18th century in particular. Dendrochronological data confirmed this general tendency in the mentioned period. Analysis of SPI (including its lowest values, i.e. droughts) showed that the long-term frequency of droughts in Poland has been stable in the last two or three centuries. Extreme and severe droughts were most frequent in the coastal part of Poland and in Silesia. Most droughts had a duration of 2 months (about 60 %–70 %) or 3–4 months (10 %–20 %). Frequencies of droughts with a duration of 5-or-more months were lower than 10 %. The frequency of droughts of all categories in Poland in the instrumental period 1722–2015 was greatest in winter, while in the documentary evidence (1451–1800) droughts in this season are rarely mentioned. The occurrence of negative pointer years (a good proxy for droughts) was compared with droughts delimited based on documentary and instrumental data. A good correspondence was found between the timing of occurrence of droughts identified using all three kinds of data (sources).
    Print ISSN: 1814-9324
    Electronic ISSN: 1814-9332
    Topics: Geosciences
    Published by Copernicus on behalf of European Geosciences Union.
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  • 6
    Publication Date: 2017-02-04
    Print ISSN: 1612-4669
    Electronic ISSN: 1612-4677
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Published by Springer
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  • 7
    Publication Date: 2010-12-21
    Print ISSN: 0020-7128
    Electronic ISSN: 1432-1254
    Topics: Geography , Physics
    Published by Springer
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  • 8
  • 9
    Publication Date: 2009-12-01
    Description: In this study grid data of daily maximum and minimum air temperatures taken from the NCEP/NCAR reanalysis for the territory of Poland for the years 1951-2005 have been used as a basis for an analysis of the spatial distribution of daily maximum and minimum air temperature, the frequency of characteristic days and the variability of these parameters in the period analysed. The results obtained were then compared to the variability in atmospheric circulation in Europe, described by the North Atlantic Oscillation (NAO) index.
    Print ISSN: 2080-7686
    Electronic ISSN: 2300-8490
    Topics: Geography
    Published by De Gruyter
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  • 10
    Publication Date: 2018-12-01
    Description: The aim of the studies was to evaluate the usefulness of the microscopic features of wood in characterising the climatic conditions of a period for which only proxy data are available. Samples were taken from historical wood from Koronowo collegiate church and from a living Scots pine tree growing in the Toruń-Wrzosy site. All measurements were performed using ImageJ software. The dendroclimatological analysis was carried out in the program DendroClim2002. The results show a correlation between the microscopic features of wood and climatic conditions. For the period 1951–2000 the maximum optical density of pine wood depends on average May air temperature and June precipitation, with correlation coefficients of −0.32 and −0.29, respectively. A similar correlation was found for mean maximum and minimum temperatures in May; -0.35 and -0.37, respectively. Additional correlations between selected meteorological elements and the maximum optical density of the wood were found using 30-year moving averages and moving intervals.
    Print ISSN: 2080-7686
    Electronic ISSN: 2300-8490
    Topics: Geography
    Published by De Gruyter
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