Evaluation of four global reanalysis products using in-situ observations in the Amundsen Sea Embayment, Antarctica

Jones, R. W.; Renfrew, I. A.; Orr, A. ORCID: https://orcid.org/0000-0001-5111-8402; Webber, B. G. M.; Holland, D. M.; Lazzara, M. A.. 2016 Evaluation of four global reanalysis products using in-situ observations in the Amundsen Sea Embayment, Antarctica. Journal of Geophysical Research: Atmospheres, 121 (11). 6240-6257. https://doi.org/10.1002/2015JD024680

Before downloading, please read NORA policies.

Preview

Text Jones_et_al-2016-Journal_of_Geophysical_Research__Atmospheres.pdf - Published Version Available under License Creative Commons Attribution 4.0. Download (2MB) | Preview

Abstract/Summary

The glaciers within the Amundsen Sea Embayment (ASE), West Antarctica, are amongst the most rapidly retreating in Antarctica. Meteorological reanalysis products are widely used to help understand and simulate the processes causing this retreat. Here we provide an evaluation against observations of four of the latest global reanalysis products within the ASE region – the ECMWF Interim Re-analysis (ERA-I), Japanese 55-year Reanalysis (JRA-55), Climate Forecast System Reanalysis (CFSR) and Modern Era Retrospective-Analysis for Research and Applications (MERRA). The observations comprise data from four automatic weather stations (AWS), three research-vessel cruises and a new set of 38 radiosondes all within the period 2009-2014. All four reanalyses produce 2 m temperature fields that are colder than AWS observations, with the biases varying from approximately -1.8 °C (ERA-I) to -6.8 °C (MERRA). Over the Amundsen Sea, spatially averaged summertime biases are between -0.4 °C (JRA-55) and -2.1 °C (MERRA) with notably larger cold biases close to the continent (up to -6 °C) in all reanalyses. All four reanalyses underestimate near surface wind speed at high wind speeds (>15 m s-1) and exhibit dry biases and relatively large root-mean-square errors (RMSE) in specific humidity. A comparison to the radiosonde soundings shows that the cold, dry bias at the surface extends into the lower troposphere; here ERA-I and CFSR reanalyses provide the most accurate profiles. The reanalyses generally contain larger temperature and humidity biases, (and RMSE) when a temperature inversion is observed; and contain larger wind speed biases (~2 to 3 m s-1) when a low-level jet is observed

Item Type:	Publication - Article
Digital Object Identifier (DOI):	https://doi.org/10.1002/2015JD024680
Programmes:	BAS Programmes > BAS Programmes 2015 > Atmosphere, Ice and Climate
ISSN:	2169897X
Additional Keywords:	reanalyses, Antarctic, Amundsen, radiosondes, Pine Island Glacier
Date made live:	31 May 2016 10:37 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/513726

Actions (login required)

View Item

Document Downloads

More statistics for this item...