An ERA40-based atmospheric forcing for global ocean circulation models

Type Article
Date 2010
Language English
Author(s) Brodeau Laurent1, Barnier Bernard, Treguier Anne-Marie2, Penduff Thierry4, Gulev Sergei3
Affiliation(s) 1 : CNRS UJF INPG, LEGI, Lab Phys & Ocean, UMR 5519, F-38041 Grenoble, France.
2 : CNRS IFREMER IRD UBO, LPO, UMR 6523, F-29280 Plouzane, France.
3 : Russian Acad Sci, PP SIO, Moscow 117218, Russia.
4 : Florida State Univ, Dept Oceanog, Tallahassee, FL 32306 USA.
Source Ocean Modelling (1463-5003) (Elsevier Sci Ltd), 2010 , Vol. 31 , N. 3-4 , P. 88-104
DOI 10.1016/j.ocemod.2009.10.005
WOS© Times Cited 316
Keyword(s) Ocean, Hindcast, Atmospheric forcing, Air sea fluxes, Weather reanalyzes, Satellite
Abstract We develop, calibrate and test a dataset intended to drive global ocean hindcasts simulations of the last five decades. This dataset provides surface meteorological variables needed to estimate air-sea fluxes and is built from 6-hourly surface atmospheric state variables of ERA40. We first compare the raw fields of ERA40 to the CORE.v1 clataset of Large and Yeager (2004). used here as a reference, and discuss our choice to use daily radiative fluxes and monthly precipitation products extracted from satellite data rather than their ERA40 counterparts. Both datasets lead to excessively high global imbalances of heat and freshwater fluxes when tested with a prescribed climatological sea surface temperature. After identifying unrealistic time discontinuities (induced by changes in the nature of assimilated observations) and obvious global and regional biases in ERA40 fields (by comparison to high quality observations), we propose a set of corrections. Tropical surface air humidity is decreased from 1979 onward, representation of Arctic surface air temperature is improved using recent observations and the wind is globally increased. These corrections lead to a significant decrease of the excessive positive global imbalance of heat. Radiation and precipitation fields are then submitted to a small adjustment (in zonal mean) that yields a near-zero global imbalance of heat and freshwater. A set of 47-year-long simulations is carried out with the coarse-resolution (2 degrees x 2 degrees) version of the NEMO OGCM to assess the sensitivity of the model to the proposed corrections. Model results show that each of the proposed correction contributes to improve the representation of central features of the global ocean circulation. (c) 2009 Elsevier Ltd. All rights reserved.
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