The Arctic System Reanalysis, Version 2Source: Bulletin of the American Meteorological Society:;2017:;volume 099:;issue 004::page 805Author:Bromwich, D. H.
,
Wilson, A. B.
,
Bai, L.
,
Liu, Z.
,
Barlage, M.
,
Shih, C.-F.
,
Maldonado, S.
,
Hines, K. M.
,
Wang, S.-H.
,
Woollen, J.
,
Kuo, B.
,
Lin, H.-C.
,
Wee, T.-K.
,
Serreze, M. C.
,
Walsh, J. E.
DOI: 10.1175/BAMS-D-16-0215.1Publisher: American Meteorological Society
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.
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contributor author | Bromwich, D. H. | |
contributor author | Wilson, A. B. | |
contributor author | Bai, L. | |
contributor author | Liu, Z. | |
contributor author | Barlage, M. | |
contributor author | Shih, C.-F. | |
contributor author | Maldonado, S. | |
contributor author | Hines, K. M. | |
contributor author | Wang, S.-H. | |
contributor author | Woollen, J. | |
contributor author | Kuo, B. | |
contributor author | Lin, H.-C. | |
contributor author | Wee, T.-K. | |
contributor author | Serreze, M. C. | |
contributor author | Walsh, J. E. | |
date accessioned | 2019-09-19T10:06:30Z | |
date available | 2019-09-19T10:06:30Z | |
date copyright | 12/11/2017 12:00:00 AM | |
date issued | 2017 | |
identifier other | bams-d-16-0215.1.pdf | |
identifier uri | http://yetl.yabesh.ir/yetl1/handle/yetl/4261616 | |
description 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 | |
title | The Arctic System Reanalysis, Version 2 | |
type | Journal Paper | |
journal volume | 99 | |
journal issue | 4 | |
journal title | Bulletin of the American Meteorological Society | |
identifier doi | 10.1175/BAMS-D-16-0215.1 | |
journal fristpage | 805 | |
journal lastpage | 828 | |
tree | Bulletin of the American Meteorological Society:;2017:;volume 099:;issue 004 | |
contenttype | Fulltext |