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    Horizontal and Vertical Structure of Cross-Equatorial Wave Propagation 

    Source: Journal of the Atmospheric Sciences:;1994:;Volume( 051 ):;issue: 011:;page 1417
    Author(s): Tomas, Robert A.; Webster, Peter J.
    Publisher: American Meteorological Society
    Abstract: Observational evidence of interhemispheric wave propagation through the equatorial upper-tropospheric mean westerlies in the eastern Pacific Ocean is found in nine years (1980/81 to 1988/89) of European Centre for Medium-Range ...
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    The Transient Atmospheric Circulation Response to North Atlantic SST and Sea Ice Anomalies 

    Source: Journal of Climate:;2007:;volume( 020 ):;issue: 018:;page 4751
    Author(s): Deser, Clara; Tomas, Robert A.; Peng, Shiling
    Publisher: American Meteorological Society
    Abstract: The objective of this study is to investigate the transient evolution of the wintertime atmospheric circulation response to imposed patterns of SST and sea ice extent anomalies in the North Atlantic sector using a large ...
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    The Role of Ocean–Atmosphere Coupling in the Zonal-Mean Atmospheric Response to Arctic Sea Ice Loss 

    Source: Journal of Climate:;2014:;volume( 028 ):;issue: 006:;page 2168
    Author(s): Deser, Clara; Tomas, Robert A.; Sun, Lantao
    Publisher: American Meteorological Society
    Abstract: he role of ocean?atmosphere coupling in the zonal-mean climate response to projected late twenty-first-century Arctic sea ice loss is investigated using Community Climate System Model version 4 (CCSM4) at 1° spatial ...
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    Mechanisms of Stratospheric and Tropospheric Circulation Response to Projected Arctic Sea Ice Loss 

    Source: Journal of Climate:;2015:;volume( 028 ):;issue: 019:;page 7824
    Author(s): Sun, Lantao; Deser, Clara; Tomas, Robert A.
    Publisher: American Meteorological Society
    Abstract: he impact of projected Arctic sea ice loss on the atmospheric circulation is investigated using the Whole Atmosphere Community Climate Model (WACCM), a model with a well-resolved stratosphere. Two 160-yr simulations are ...
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    Arctic Inversion Strength in Climate Models 

    Source: Journal of Climate:;2011:;volume( 024 ):;issue: 017:;page 4733
    Author(s): Medeiros, Brian; Deser, Clara; Tomas, Robert A.; Kay, Jennifer E.
    Publisher: American Meteorological Society
    Abstract: ecent work indicates that climate models have a positive bias in the strength of the wintertime low-level temperature inversion over the high-latitude Northern Hemisphere. It has been argued this bias leads to underestimates ...
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    Air–Sea Turbulent Heat Fluxes in Climate Models and Observational Analyses: What Drives Their Variability? 

    Source: Journal of Climate:;2019:;volume 032:;issue 008:;page 2397
    Author(s): Small, R. Justin; Bryan, Frank O.; Bishop, Stuart P.; Tomas, Robert A.
    Publisher: American Meteorological Society
    Abstract: AbstractA traditional view is that the ocean outside of the tropics responds passively to atmosphere forcing, which implies that air?sea heat fluxes are mainly driven by atmosphere variability. This paper tests this viewpoint ...
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    Climatological Characteristics of Arctic and Antarctic Surface-Based Inversions 

    Source: Journal of Climate:;2011:;volume( 024 ):;issue: 019:;page 5167
    Author(s): Zhang, Yehui; Seidel, Dian J.; Golaz, Jean-Christophe; Deser, Clara; Tomas, Robert A.
    Publisher: American Meteorological Society
    Abstract: urface-based inversions (SBIs) are frequent features of the Arctic and Antarctic atmospheric boundary layer. They influence vertical mixing of energy, moisture and pollutants, cloud formation, and surface ozone destruction. ...
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    ENSO and Pacific Decadal Variability in the Community Climate System Model Version 4 

    Source: Journal of Climate:;2011:;volume( 025 ):;issue: 008:;page 2622
    Author(s): Deser, Clara; Phillips, Adam S.; Tomas, Robert A.; Okumura, Yuko M.; Alexander, Michael A.; Capotondi, Antonietta; Scott, James D.; Kwon, Young-Oh; Ohba, Masamichi
    Publisher: American Meteorological Society
    Abstract: his study presents an overview of the El Niño?Southern Oscillation (ENSO) phenomenon and Pacific decadal variability (PDV) simulated in a multicentury preindustrial control integration of the NCAR Community Climate System ...
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