The Arctic System Reanalysis, Version 2

Author:

Bromwich D. H.1,Wilson A. B.2,Bai L.2,Liu Z.3,Barlage M.4,Shih C.-F.5,Maldonado S.1,Hines K. M.2,Wang S.-H.2,Woollen J.6,Kuo B.7,Lin H.-C.3,Wee T.-K.8,Serreze M. C.9,Walsh J. E.10

Affiliation:

1. Polar Meteorology Group, Byrd Polar and Climate Research Center, and Atmospheric Sciences Program, Department of Geography, The Ohio State University, Columbus, Ohio

2. Polar Meteorology Group, Byrd Polar and Climate Research Center, The Ohio State University, Columbus, Ohio

3. Mesoscale and Microscale Meteorology Laboratory, National Center for Atmospheric Research, Boulder, Colorado

4. Research Applications Laboratory, National Center for Atmospheric Research, Boulder, Colorado

5. Computational Information Systems Laboratory, National Center for Atmospheric Research, Boulder, Colorado

6. National Centers for Environmental Prediction, College Park, Maryland

7. UCAR Community Programs, University Corporation for Atmospheric Research, Boulder, Colorado

8. Constellation Observing System for Meteorology, Ionosphere, and Climate, University Corporation for Atmospheric Research, Boulder, Colorado

9. National Snow and Ice Data Center, Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, Colorado

10. International Arctic Research Center, University of Alaska Fairbanks, Fairbanks, Alaska

Abstract

AbstractThe Arctic is a vital component of the global climate, and its rapid environmental evolution is an important element of climate change around the world. To detect and diagnose the changes occurring to the coupled Arctic climate system, a state-of-the-art synthesis for assessment and monitoring is imperative. This paper presents the Arctic System Reanalysis, version 2 (ASRv2), a multiagency, university-led retrospective analysis (reanalysis) of the greater Arctic region using blends of the polar-optimized version of the Weather Research and Forecasting (Polar WRF) Model and WRF three-dimensional variational data assimilated observations for a comprehensive integration of the regional climate of the Arctic for 2000–12. New features in ASRv2 compared to version 1 (ASRv1) include 1) higher-resolution depiction in space (15-km horizontal resolution), 2) updated model physics including subgrid-scale cloud fraction interaction with radiation, and 3) a dual outer-loop routine for more accurate data assimilation. ASRv2 surface and pressure-level products are available at 3-hourly and monthly mean time scales at the National Center for Atmospheric Research (NCAR). Analysis of ASRv2 reveals superior reproduction of near-surface and tropospheric variables. Broadscale analysis of forecast precipitation and site-specific comparisons of downward radiative fluxes demonstrate significant improvement over ASRv1. The high-resolution topography and land surface, including weekly updated vegetation and realistic sea ice fraction, sea ice thickness, and snow-cover depth on sea ice, resolve finescale processes such as topographically forced winds. Thus, ASRv2 permits a reconstruction of the rapid change in the Arctic since the beginning of the twenty-first century–complementing global reanalyses. ASRv2 products will be useful for environmental models, verification of regional processes, or siting of future observation networks.

Publisher

American Meteorological Society

Subject

Atmospheric Science

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