Publication Abstracts

Foster et al. 1996

Foster, J., G. Liston, R. Koster, R. Essery, H. Behr, L. Dumenil, D. Verseghy, S. Thompson, D. Pollard, and J.L. Cohen, 1996: Snow cover and snow mass intercomparisons of general circulation models and remotely sensed datasets. J. Climate, 9, 409-426, doi:10.1175/1520-0442(1996)009<0409:SCASMI>2.0.CO;2.

Confirmation of the ability of general circulation models (GCMs) to accurately represent snow cover and snow mass distributions is vital for climate studies. There must be a high degree of confidence that what is being predicted by the models is reliable, since realistic results cannot be assured unless they are tested against results from observed data or other available datasets. In this study, snow output from seven GCMs and passive-microwave snow data derived from the Nimbus-7 Scanning Multichannel Microwave Radiometer (SMMR) are intercompared. National Oceanic and Atmospheric Administration satellite data are used as the standard of reference for snow extent observations and the U.S. Air Force snow depth climatology is used as the standard for snow mass. The reliability of the SMMR snow data needs to be verified, as well, because currently this is the only available dataset that allows for yearly and monthly variations in snow depth. [The GCMs employed in this investigation are the United Kingdom Meteorological Office, Hadley Center GCM, the Max Planck Institute for Meteorology/University of Hamburg (ECHAM) GCM, the Canadian Climate Centre GCM, the National Center for Atmospheric Research (GENESIS) GCM, the Goddard Institute for Space Studies GCM, the Goddard Laboratory for Atmospheres GCM and the Goddard Coupled Climate Dynamics Group (AIRES) GCM.] Data for both North America and Eurasia are examined in an effort to assess the magnitude of spatial and temporal variations that exist between the standards of reference, the models, and passive microwave data. Results indicate that both the models and SMMR represent seasonal and year-to-year snow distributions fairly well. The passive microwave data and several of the models, however, consistently underestimate snow mass, but other models overestimate the mass of snow on the ground. The models do a better job simulating winter and summer snow conditions than in the transition months. In general, the underestimation by SMMR is caused by absorption of microwave energy by vegetation. For the GCMs, differences between observed snow conditions can be ascribed to inaccuracies in simulating surface air temperatures and precipitation fields, especially during the spring and fall.

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BibTeX Citation

  author={Foster, J. and Liston, G. and Koster, R. and Essery, R. and Behr, H. and Dumenil, L. and Verseghy, D. and Thompson, S. and Pollard, D. and Cohen, J. L.},
  title={Snow cover and snow mass intercomparisons of general circulation models and remotely sensed datasets},
  journal={J. Climate},

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RIS Citation

ID  - fo01000b
AU  - Foster, J.
AU  - Liston, G.
AU  - Koster, R.
AU  - Essery, R.
AU  - Behr, H.
AU  - Dumenil, L.
AU  - Verseghy, D.
AU  - Thompson, S.
AU  - Pollard, D.
AU  - Cohen, J. L.
PY  - 1996
TI  - Snow cover and snow mass intercomparisons of general circulation models and remotely sensed datasets
JA  - J. Climate
VL  - 9
SP  - 409
EP  - 426
DO  - 10.1175/1520-0442(1996)009%3C0409%3ASCASMI%3E2.0.CO;2
ER  -

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