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contributor authorBromwich, D. H.
contributor authorWilson, A. B.
contributor authorBai, L.
contributor authorLiu, Z.
contributor authorBarlage, M.
contributor authorShih, C.-F.
contributor authorMaldonado, S.
contributor authorHines, K. M.
contributor authorWang, S.-H.
contributor authorWoollen, J.
contributor authorKuo, B.
contributor authorLin, H.-C.
contributor authorWee, T.-K.
contributor authorSerreze, M. C.
contributor authorWalsh, J. E.
date accessioned2019-09-19T10:06:30Z
date available2019-09-19T10:06:30Z
date copyright12/11/2017 12:00:00 AM
date issued2017
identifier otherbams-d-16-0215.1.pdf
identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4261616
description abstractAbstractThe 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.
publisherAmerican Meteorological Society
titleThe Arctic System Reanalysis, Version 2
typeJournal Paper
journal volume99
journal issue4
journal titleBulletin of the American Meteorological Society
identifier doi10.1175/BAMS-D-16-0215.1
journal fristpage805
journal lastpage828
treeBulletin of the American Meteorological Society:;2017:;volume 099:;issue 004
contenttypeFulltext


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