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  • 1
    Call number: AWI A4-95-0010
    In: Antarctic research series, Vol. 61
    Type of Medium: Monograph available for loan
    Pages: XIV, 207 S. : Ill., graph. Darst. + 1 Disk.
    ISBN: 087590839X
    Series Statement: Antarctic research series 61
    Language: English
    Note: CONTENTS: The Antarctic Research Series: Statement of Objectives / Board of Associate Editors. - Preface / David H. Bromwich and Charles R. Stearns. - Monthly Mean Climatic Data for Antarctic Automatic Weather Stations / Charles R. Stearns, Linda M. Keller, George A. Weidner, and Manuela Sievers. - Katabatic Winds in Adélie Coast / Gerd Wendler, Jean Claude Andre, Paul Pettre, loan Gosink, and Thomas Parish. - Spatial and Temporal Characteristics of the Intense Katabatic Winds at Terra Nova Bay, Antarctica / David H. Bromwich, Thomas R. Parish, Andrea Pellegrini, Charles R. Stearns, and George A. Weidner. - Katabatic Winds Along the Transantarctic Mountains / Christopher J. Breckenridge, Uwe Radok, Charles R. Stearns, and David H. Bromwich. - Satellite and Automatic Weather Station Analyses of Katabatic Surges Across the Ross Ice Shelf / Jorge F. Carrasco and David H. Bromwich. - Sensible and Latent Heat Flux Estimates in Antarctica / Charles R. Stearns and George A. Weidner. - The Kernlose Winter in Adélie Coast / Gerd Wendler and Yuji Kodama. - Antarctic Climate Anomalies Surrounding the Minimum in the Southern Oscillation Index / Shawn R. Smith and Charles R. Stearns. - Variation in Aerosol Concentration Associated With a Polar Climatic Iteration / A. Hogan, D. Riley, B. B. Murphey, S. C. Barnard, and J. A. Samson. - Continuous Nanoclimate Data (1985-1988) From the Ross Desert (McMurdo Dry Valleys) Cryptoendolithic Microbial Ecosystem / Christopher P. McKay, lames A. Nienow, Michael A. Meyer, and E. lmre Friedmann.
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 2
    Publication Date: 2023-01-13
    Keywords: Air temperature at 2 m height; DATE/TIME; Event label; Punta_Dungeness; South Atlantic Ocean
    Type: Dataset
    Format: text/tab-separated-values, 1132 data points
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  • 3
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    Unknown
    PANGAEA
    In:  Supplement to: Jones, Megan E; Bromwich, David H; Nicolas, Julien P; Carrasco, Jorge; Plavcová, Eva; Zou, Xun; Wang, Sheng-Hung (2019): Sixty Years of Widespread Warming in the Southern Middle and High Latitudes (1957–2016). Journal of Climate, 32(20), 6875-6898, https://doi.org/10.1175/JCLI-D-18-0565.1
    Publication Date: 2023-01-13
    Description: 3- or 6-hourly 2-meter temperature observations were recorded at Diego Ramirez, Evangelistas, and Punta Dungeness, 3 stations in the southern South America region. These were retrieved from the Navy Weather Service of Chile and then digitized and condensed into monthly means. Diego Ramirez is located at -56.3, -68.4; Evangelistas is located at -52.2, -75.1; and Punta Dungeness is located at -52.2, -68.3. Evangelistas begins in 1901, Punta Dungeness in 1920, and Diego Ramirez in 1956.
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 4
    Publication Date: 2023-01-13
    Keywords: Air temperature at 2 m height; DATE/TIME; Diego_Ramirez2; Event label; South Pacific Ocean; SST
    Type: Dataset
    Format: text/tab-separated-values, 696 data points
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  • 5
    Publication Date: 2023-01-13
    Keywords: Air temperature at 2 m height; DATE/TIME; Evangelistas; Event label; South Pacific Ocean
    Type: Dataset
    Format: text/tab-separated-values, 1038 data points
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  • 6
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Fountain, Andrew G; Nylen, Thomas H; Monaghan, Andrew J; Basagic, Hassan J; Bromwich, David H (2010): Snow in the McMurdo Dry Valleys, Antarctica. International Journal of Climatology, 30(5), 633-642, https://doi.org/10.1002/joc.1933
    Publication Date: 2023-12-13
    Description: Snowfall was measured at 11 sites in the McMurdo Dry Valleys to determine its magnitude, its temporal changes, and spatial patterns. Annual values ranged from 3 to 50 mm water equivalent with the highest values nearest the coast and decreasing inland. A particularly strong spatial gradient exists in Taylor Valley, probably resulting from local uplift conditions at the coastal margin and valley topography that limits migration inland. More snow occurs in winter near the coast, whereas inland no seasonal pattern is discernable. This may be due, again, to local uplift conditions, which are common in winter. We find no influence of the distance to the sea ice edge. Katabatic winds play an important role in transporting snow to the valley bottoms and essentially double the precipitation. That much of the snow accumulation sublimates prior to making a hydrologic contribution underscores the notion that the McMurdo Dry Valleys are indeed an extreme polar desert.
    Keywords: Accumulation of snow in water equivalent per year; Canada_Gl; Commonw_Gl; DATE/TIME; Device type; Event label; Explorers_Cove2; Howard_Gl; International Polar Year (2007-2008); IPY; Lake_Bonney; Lake_Brownworth2; Lake_Fryxell2; Lake_Hoare2; Lake_Vanda2; Lake_Vida; Latitude of event; Longitude of event; Taylor_Gl; Taylor Valley, East Antarctica; Unmanned weather station/meteorological observation; UWST; Victoria Valley, East Antarctica; Wright Valley, East Antarctica
    Type: Dataset
    Format: text/tab-separated-values, 144 data points
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  • 7
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Speirs, Johanna C; Steinhoff, Daniel F; McGowan, Hamish A; Bromwich, David H; Monaghan, Andrew J (2010): Foehn Winds in the McMurdo Dry Valleys, Antarctica: The Origin of Extreme Warming Events. Journal of Climate, 23(13), 3577-3598, https://doi.org/10.1175/2010JCLI3382.1
    Publication Date: 2023-12-13
    Description: Foehn winds resulting from topographic modification of airflow in the lee of mountain barriers are frequently experienced in the McMurdo Dry Valleys (MDVs) of Antarctica. Strong foehn winds in the MDVs cause dramatic warming at onset and have significant effects on landscape forming processes; however, no detailed scientific investigation of foehn in the MDVs has been conducted. As a result, they are often misinterpreted as adiabatically warmed katabatic winds draining from the polar plateau. Herein observations from surface weather stations and numerical model output from the Antarctic Mesoscale Prediction System (AMPS) during foehn events in the MDVs are presented. Results show that foehn winds in the MDVs are caused by topographic modification of south-southwesterly airflow, which is channeled into the valleys from higher levels. Modeling of a winter foehn event identifies mountain wave activity similar to that associated with midlatitude foehn winds. These events are found to be caused by strong pressure gradients over the mountain ranges of the MDVs related to synoptic-scale cyclones positioned off the coast of Marie Byrd Land. Analysis of meteorological records for 2006 and 2007 finds an increase of 10% in the frequency of foehn events in 2007 compared to 2006, which corresponds to stronger pressure gradients in the Ross Sea region. It is postulated that the intra- and interannual frequency and intensity of foehn events in the MDVs may therefore vary in response to the position and frequency of cyclones in the Ross Sea region.
    Keywords: Beacon_Valley2; Canada_Gl; Comment; Commonw_Gl; DATE/TIME; Date/time end; Event label; Explorers_Cove2; Howard_Gl; Humidity, relative, minimum; International Polar Year (2007-2008); IPY; Lake_Bonney; Lake_Fryxell2; Lake_Hoare2; Lake_Vanda2; Lake_Vida; McMurdo Dry Valleys, southern Victorica Land, Antarctica; Station label; Taylor_Gl; Taylor Valley, East Antarctica; Temperature, air, maximum; Temperature, air, minimum; Unmanned weather station/meteorological observation; UWST; Victoria Valley, East Antarctica; Wind direction; Wind speed, gust; Wright Valley, East Antarctica
    Type: Dataset
    Format: text/tab-separated-values, 82 data points
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  • 8
    Publication Date: 2024-03-18
    Keywords: -; Accumulation of snow/ice per year; Calculated; Calculated average/mean values; Comment; Country; Deuterium excess; Deuterium excess, maximum; Deuterium excess, minimum; Deuterium excess, standard deviation; Distance; Ice floe type; International Polar Year (2007-2008); IPY; LATITUDE; LONGITUDE; Number of values averaged at depth horizon; ORDINAL NUMBER; Quality code; Reference/source; Sample code/label; Sampling date; Temperature, ice/snow; δ18O, maximum; δ18O, minimum; δ18O, standard deviation; δ18O, water; δ Deuterium; δ Deuterium, maximum; δ Deuterium, minimum; δ Deuterium, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 16434 data points
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  • 9
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 328 (1987), S. 51-54 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Observational and theoretical studies of gravity-driven slope flows (katabatic winds) are numerous. Ball8 points out that the magnitude of terrain-induced pressure gradient is directly pro-portional to both the steepness of the terrain and the strength of the temperature inversion in the lower ...
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 343 (1990), S. 627-629 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] TABLE 1 Annual zonal averages of meridional moisture transport and its convergence Transport (kg rrT Convergence (kg m 2 yr [P-E] Latitude Latitude °S PO HR Belt°S PO HR BR 50 -17 -10.5 50-60 290 160 452 60 -10 -6.7 60-70 270 133 322 70 -3 -3.7 70-80 90 97 183 ...
    Type of Medium: Electronic Resource
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