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  • 1
    Monograph available for loan
    Monograph available for loan
    The last great ice sheets (1981)
    New York [u.a.] : Wiley
    Details Availability
    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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  • 2
    Monograph available for loan
    Monograph available for loan
    Berliner Wetterkarte im Jahre 1997 : tägliche Wetterkarten (Boden, 850 hPa, 500 hPa, europäisches Wetterbild), monatliche und jährliche Witterungsübersichten und Tabellen sowie wissenschaftliche Aufsätze (1997)
    Berlin : Reimer
    Associated volumes
    Details Availability
    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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  • 3
    Monograph available for loan
    Monograph available for loan
    Holocene Climatic Variations : their pattern and possible cause (1973)
    Washington
    Associated volumes
    Details Availability
    Call number: AWI G5-99-0095
    In: Quaternary Research, Volume 3, Issue 2
    Type of Medium: Monograph available for loan
    Pages: Seite 155-205 , Illustrationen , 30 cm
    ISSN: 0033-5894 (Print) , 1096-0287 (Online)
    Series Statement: Quaternary Research 3,2
    Language: English
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  • 4
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    Regional climate control of glaciers in New Zealand and Europe during the pre-industrial Holocene (2012)
    Springer Nature
    Details
    Publication Date: 2012-09-01
    Description: Regional climate control of glaciers in New Zealand and Europe during the pre-industrial Holocene Nature Geoscience 5, 627 (2012). doi:10.1038/ngeo1548 Authors: Aaron E. Putnam, Joerg M. Schaefer, George H. Denton, David J. A. Barrell, Robert C. Finkel, Bjørn G. Andersen, Roseanne Schwartz, Trevor J. H. Chinn & Alice M. Doughty Mountain glaciers worldwide have undergone net recession over the past century in response to atmospheric warming, but the extent to which this warming reflects natural versus anthropogenic climate change remains uncertain. Between about 11,500 years ago and the nineteenth century, progressive atmospheric cooling over the European Alps induced glacier expansion, culminating with several large-scale advances during the seventeen to nineteenth centuries. However, it is unclear whether this glacier behaviour reflects global or a more regional forcing. Here we reconstruct glacier fluctuations in the Southern Alps of New Zealand for the past 11,000 years using 10Be exposure ages. We use those fluctuations to estimate the associated temperature variations. On orbital to submillennial timescales, changes in glacier snowlines in New Zealand were linked to regional climate and oceanographic variability and were asynchronous with snowline variations in European glaciers. We attribute this asynchrony to the migration of the intertropical convergence zone. In light of this persistent asynchrony, we suggest that the net glacier recession and atmospheric warming in both regions over the past century is anomalous in the context of earlier Holocene variability and corresponds with anthropogenic emissions of greenhouse gases.
    Print ISSN: 1752-0894
    Electronic ISSN: 1752-0908
    Topics: Geosciences
    Published by Springer Nature
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  • 5
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    Palaeoclimate: East Antarctic retreat (2011)
    Springer Nature
    Details
    Publication Date: 2011-03-01
    Description: Palaeoclimate: East Antarctic retreat Nature Geoscience 4, 135 (2011). doi:10.1038/ngeo1096 Author: George H. Denton The contribution of the East Antarctic ice sheet to the 120 m of sea-level rise since the Last Glacial Maximum is unclear. New terrestrial and marine data suggest the thinning of East Antarctic ice was responsible for only a metre of this rise.
    Print ISSN: 1752-0894
    Electronic ISSN: 1752-0908
    Topics: Geosciences
    Published by Springer Nature
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  • 6
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    Accumulation and marine forcing of ice dynamics in the western Ross Sea during the last deglaciation (2015)
    Springer Nature
    Details
    Publication Date: 2015-07-31
    Description: Nature Geoscience 8, 625 (2015). doi:10.1038/ngeo2478 Authors: Brenda L. Hall, George H. Denton, Stephanie L. Heath, Margaret S. Jackson & Tobias N. B. Koffman The grounding line of the ice sheet in the Ross Sea, Antarctica, retreated between the Last Glacial Maximum and the present. However, the timing of the retreat and the interplay of factors controlling ice stability in this region remain uncertain. Here we use 180 radiocarbon dates to reconstruct the chronology of moraine construction on the headlands adjacent to western McMurdo Sound. On the basis of these dates we then assess the timing of ice expansion and retreat in the Ross drainage system that is fed from both the East and West Antarctic ice sheets. We find that grounded ice in the western Ross Sea achieved its greatest thickness and extent during the last termination, between 12,800 and 18,700 years ago. Maximum ice thickness at our site coincides with a period of high accumulation as recorded by the West Antarctic Ice Sheet Divide ice core. Recession of the ice sheet from the headland moraines began about 12,800 years ago, despite continued high accumulation and the expansion of land-based glaciers at this time. We therefore suggest that the grounding-line retreat reflects an increased marine influence as sea levels rose and the ocean warmed. We suggest that future instability in the ice sheet grounding line may occur whenever the ocean forcing is stronger than forcing from accumulation.
    Print ISSN: 1752-0894
    Electronic ISSN: 1752-0908
    Topics: Geosciences
    Published by Springer Nature
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  • 7
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    Correlation of Glacier ELA/Snowlines & Temperature Station data with ERA5 Temperature and Wind Speed, 1979 to 2017 (2022)
    PANGAEA
    Details
    Publication Date: 2024-04-20
    Description: This dataset contains the gridded correlation results from a study that sought to better understand the climatic footprint monitored by antipodal mid-latitude glacier populations. Understanding the links between glaciers and climate is critical for accurately interpreting contemporary cryosphere changes, and interrogating the causes of past glacier behavior. However, work is still needed to refine the extent to which they capture regional to hemisphere-scale atmospheric processes. A Pearson's correlation was performed between yearly summer seasonal data from the ERA5 gridded reconstructions of global temperature and wind changes on each available ERA5 pressure level and yearly glacier snowline/ELA elevations in the Southern Alps of New Zealand and in the European Alps. December-Febuary austral summer data was correlated with the Southern Alps records and June-August Northern Hemisphere summer data was correlated with the European Alps. The ERA5 input dataset was regridded onto a new monthly axis representing the true month lengths. Then the weighted seasonal average (December-February and June-August) was calculated. Individuals glaciers with Equilibrium Line Altitude (ELA; European Alps) and End of Summer Snowlines (EOSS; Southern Alps) were selected with respective records covering at least 80% of the 1979-2017/15 analysis period. The records from each glacier were then standardized and an EOF analysis was performed to obtain each location's First Principle Component for input into the Pearson's Correlation. A nearly identical set of analyses was performed using weather stations temperature data instead of glacier ELA/snowlines. The New Zealand station equivalent is from the National Institute of Water and Atmospheric Research (NIWA) New Zealand seven-station (NZ7S) series. The European Alps equivalent is from the HistAlp regional weather station syntheses. This companion analysis allows the glacier's ability to record the climate to be compared to that of meteorological instruments.
    Keywords: Alps; Binary Object; Binary Object (File Size); correlation; ERA5; European Alps; File content; glacier; New Zealand; Southern Hemisphere Westerly Winds; Westerlies
    Type: Dataset
    Format: text/tab-separated-values, 14 data points
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  • 8
    Electronic Resource
    Electronic Resource
    Permafrost oxygen isotope ratios and chronology of three cores from Antarctica (1976)
    [s.l.] : Nature Publishing Group
    Nature 261 (1976), S. 547-550 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Permafrost core sediments, associated with the last intrusion of the Ross Ice Shelf in the New Harbor region, were deposited in marine (0–85 m deep) as well as freshwater environments (100–125 m). Oxygen isotope ratio measurements on these cores provide palaeoclimatic information and ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/261547a0
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  • 9
    Electronic Resource
    Electronic Resource
    Interhemispheric climate links revealed by a late-glacial cooling episode in southern Chile (2001)
    [s.l.] : Macmillian Magazines Ltd.
    Nature 409 (2001), S. 804-808 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Understanding the relative timings of climate events in the Northern and Southern hemispheres is a prerequisite for determining the causes of abrupt climate changes. But climate records from the Patagonian Andes and New Zealand for the period of transition from glacial to interglacial ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/35057252
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  • 10
    Electronic Resource
    Electronic Resource
    Preservation of Miocene glacier ice in East Antarctica (1995)
    [s.l.] : Nature Publishing Group
    Nature 376 (1995), S. 412-414 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Beacon valley (77° S, 161°E) is near the peripheral Taylor dome of the East Antarctic ice sheet. The present-day mean annual temperature is -30 to -35 °C and precipitation is less than 10 mm water equivalent per year11'12. The valley is bordered by mountains rising to ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/376412a0
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