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    Momentum, Heat, and Moisture Budgets of the Katabatic Wind Layer over a Midlatitude Glacier in Summer 

    Source: Journal of Applied Meteorology:;1997:;volume( 036 ):;issue: 006:;page 763
    Author(s): van den Broeke, Michiel R.
    Publisher: American Meteorological Society
    Abstract: In the summer of 1994, meteorological measurements were performed on Pasterze Glacier in the eastern Alps. One of the most remarkable observations concerning the observed climate was the persistent glacier wind. On the ...
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    On the Interpretation of Antarctic Temperature Trends 

    Source: Journal of Climate:;2000:;volume( 013 ):;issue: 021:;page 3885
    Author(s): van den Broeke, Michiel R.
    Publisher: American Meteorological Society
    Abstract: Determining the rate of atmospheric warming in Antarctica is hampered by the brevity of the temperature records (<50 years), which still contain signals of decadal circulation variability in the Southern Hemisphere. In ...
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    Assessing and Improving the Quality of Unattended Radiation Observations in Antarctica 

    Source: Journal of Atmospheric and Oceanic Technology:;2004:;volume( 021 ):;issue: 009:;page 1417
    Author(s): van den Broeke, Michiel; van As, Dirk; Reijmer, Carleen; van de Wal, Roderik
    Publisher: American Meteorological Society
    Abstract: The quality of atmospheric radiation measurements made at automatic weather stations (AWSs) in Antarctica is assessed. The AWSs are placed on the coastal ice shelf in the katabatic wind zone and on the high Antarctic ...
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    Simulation of Atmospheric Circulation during the GIMEX 91 Experiment Using a Meso-γ Primitive Equations Model 

    Source: Journal of Climate:;1995:;volume( 008 ):;issue: 011:;page 2843
    Author(s): Gallée, Hubert; Fontaine de Ghélin, Olivier; van den Broeke, Michiel R.
    Publisher: American Meteorological Society
    Abstract: A meso-?-scale atmospheric model has been used to simulate atmospheric circulations observed during the Greenland Ice Margin EXperiment (GIMEX). The simulations shown here are two-dimensional and cover the 12?13 July 1991 ...
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    Greenland Surface Mass Balance as Simulated by the Community Earth System Model. Part II: Twenty-First-Century Changes 

    Source: Journal of Climate:;2013:;volume( 027 ):;issue: 001:;page 215
    Author(s): Vizcaíno, Miren; Lipscomb, William H.; Sacks, William J.; van den Broeke, Michiel
    Publisher: American Meteorological Society
    Abstract: his study presents the first twenty-first-century projections of surface mass balance (SMB) changes for the Greenland Ice Sheet (GIS) with the Community Earth System Model (CESM), which includes a new ice sheet component. ...
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    Quantifying Rainfall in Greenland: A Combined Observational and Modeling Approach 

    Source: Journal of Applied Meteorology and Climatology:;2021:;volume( 060 ):;issue: 008:;page 1171
    Author(s): Huai, Baojuan;van den Broeke, Michiel R.;Reijmer, Carleen H.;Cappellen, John
    Publisher: American Meteorological Society
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    Representation of Antarctic Katabatic Winds in a High-Resolution GCM and a Note on Their Climate Sensitivity 

    Source: Journal of Climate:;1997:;volume( 010 ):;issue: 012:;page 3111
    Author(s): van den Broeke, Michiel R.; van de Wal, Roderik S. W.; Wild, Martin
    Publisher: American Meteorological Society
    Abstract: A high-resolution GCM (ECHAM-3 T106, resolution 1.1° ? 1.1°) is found to simulate many characteristic features of the Antarctic climate. The position and depth of the circumpolar storm belt, the semiannual cycle of the ...
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    Greenland Surface Mass Balance as Simulated by the Community Earth System Model. Part I: Model Evaluation and 1850–2005 Results 

    Source: Journal of Climate:;2013:;volume( 026 ):;issue: 020:;page 7793
    Author(s): Vizcaíno, Miren; Lipscomb, William H.; Sacks, William J.; van Angelen, Jan H.; Wouters, Bert; van den Broeke, Michiel R.
    Publisher: American Meteorological Society
    Abstract: he modeling of the surface mass balance (SMB) of the Greenland Ice Sheet (GIS) requires high-resolution models in order to capture the observed large gradients in the steep marginal areas. Until now, global climate models ...
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    CORRIGENDUM 

    Source: Journal of Climate:;2014:;volume( 027 ):;issue: 023:;page 8979
    Author(s): Lenaerts, Jan T. M.; van den Broeke, Michiel R.; van Wessem, Jan M.; van de Berg, Willem Jan; van Meijgaard, Erik; van Ulft, Lambertus H.; Schaefer, Marius
    Publisher: American Meteorological Society
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    Extreme Precipitation and Climate Gradients in Patagonia Revealed by High-Resolution Regional Atmospheric Climate Modeling 

    Source: Journal of Climate:;2014:;volume( 027 ):;issue: 012:;page 4607
    Author(s): Lenaerts, Jan T. M.; van den Broeke, Michiel R.; van Wessem, Jan M.; van de Berg, Willem Jan; van Meijgaard, Erik; van Ulft, Lambertus H.; Schaefer, Marius
    Publisher: American Meteorological Society
    Abstract: his study uses output of a high-resolution (5.5 km) regional atmospheric climate model to describe the present-day (1979?2012) climate of Patagonia, with a particular focus on the surface mass balance (SMB) of the Patagonian ...
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