A mechanistic analysis of tropical Pacific dynamic sea level in GFDL-OM4 under OMIP-I and OMIP-II forcings

نویسندگان

چکیده

Abstract. The sea level over the tropical Pacific is a key indicator reflecting vertically integrated heat distribution ocean. Here, we use Geophysical Fluid Dynamics Laboratory global ocean–sea ice model (GFDL-OM4) forced by both Coordinated Ocean-Ice Reference Experiment (CORE) and Japanese 55-year Reanalysis (JRA-55)-based surface dataset for driving models (JRA55-do) atmospheric states (Ocean Model Intercomparison Project (OMIP) versions I II) to evaluate performance biases compared against available observations. We find persisting mean state dynamic (DSL) bias along 9∘ N even with updated wind forcing in JRA55-do relative CORE. related stress geostrophic currents 4 latitudinal band. simulation significantly reduces DSL trend northern In CORE forcing, anomalous westerly eastern causes an underestimated across entire basin 10∘ N. also identify easterly 20∘ CORE, thus motivating future improvement. JRA55-do, accurate Rossby wave initiated at seasonal timescale corrects biased variability of equatorial countercurrent simulation. Both generate realistic variation during El Niño. asymmetry pattern on two sides Equator strongly curl that follows pressure evolution

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ژورنال

عنوان ژورنال: Geoscientific Model Development

سال: 2021

ISSN: ['1991-9603', '1991-959X']

DOI: https://doi.org/10.5194/gmd-14-2471-2021