The Met Office Unified Model Global Atmosphere 7.0/7.1 and JULES Global Land 7.0 configurations

We describe Global Atmosphere 7.0 and Global Land 7.0 (GA7.0/GL7.0), the latest science configurations of the Met Office Unified Model (UM) and the Joint UK Land Environment Simulator (JULES) land surface model developed for use across weather and climate timescales. GA7.0 and GL7.0 include incremen...

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Veröffentlicht in:Geoscientific Model Development 2019-05, Vol.12 (5), p.1909-1963
Hauptverfasser: Walters, David, Baran, Anthony J, Boutle, Ian, Brooks, Malcolm, Earnshaw, Paul, Edwards, John, Furtado, Kalli, Hill, Peter, Lock, Adrian, Manners, James, Morcrette, Cyril, Mulcahy, Jane, Sanchez, Claudio, Smith, Chris, Stratton, Rachel, Tennant, Warren, Tomassini, Lorenzo, Van Weverberg, Kwinten, Vosper, Simon, Willett, Martin, Browse, Jo, Bushell, Andrew, Carslaw, Kenneth, Dalvi, Mohit, Essery, Richard, Gedney, Nicola, Hardiman, Steven, Johnson, Ben, Johnson, Colin, Jones, Andy, Jones, Colin, Mann, Graham, Milton, Sean, Rumbold, Heather, Sellar, Alistair, Ujiie, Masashi, Whitall, Michael, Williams, Keith, Zerroukat, Mohamed
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Sprache:eng
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Zusammenfassung:We describe Global Atmosphere 7.0 and Global Land 7.0 (GA7.0/GL7.0), the latest science configurations of the Met Office Unified Model (UM) and the Joint UK Land Environment Simulator (JULES) land surface model developed for use across weather and climate timescales. GA7.0 and GL7.0 include incremental developments and targeted improvements that, between them, address four critical errors identified in previous configurations: excessive precipitation biases over India, warm and moist biases in the tropical tropopause layer (TTL), a source of energy non-conservation in the advection scheme and excessive surface radiation biases over the Southern Ocean. They also include two new parametrisations, namely the UK Chemistry and Aerosol (UKCA) GLOMAP-mode (Global Model of Aerosol Processes) aerosol scheme and the JULES multi-layer snow scheme, which improve the fidelity of the simulation and were required for inclusion in the Global Atmosphere/Global Land configurations ahead of the 6th Coupled Model Intercomparison Project (CMIP6).
ISSN:1991-9603
1991-959X
1991-962X
1991-9603
1991-962X
DOI:10.5194/gmd-12-1909-2019