Matches in SemOpenAlex for { <https://semopenalex.org/work/W4283274265> ?p ?o ?g. }
- W4283274265 endingPage "998" @default.
- W4283274265 startingPage "998" @default.
- W4283274265 abstract "In this study, the Chinese Academy of Sciences’ Earth System Model Version 2 (CAS-ESM2) and its atmospheric component were evaluated for the ability to simulate the East Asian summer monsoon (EASM), in terms of climatology and composites in El Niño decaying years (EN) and La Niña years (LN). The results show that the model can realistically simulate the El Niño Southern Oscillation (ENSO) annual cycle, the interannual variation, the evolution process, and the prerequisites of ENSO, but the trend of developing and decaying is faster than that of the observations. With regard to the climatological mean state in the EASM, the coupled model run can largely improve the precipitation and 850 hPa wind simulated in the atmospheric model. Moreover, the coupled run can also reduce the mid-latitude bias in the atmospheric model simulation. Composite methods were then adopted to examine performance in different phases of the ENSO, from a mature winter to a decaying summer. The atmospheric model can well reproduce the Western North Pacific Anomalous Anticyclone (WNPAC)/Western North Pacific Anomalous Cyclone (WNPC) during EN/LN well, but the westerly/easterly anomalies and the associated precipitation anomalies over the equatorial Central Eastern Pacific are somewhat overestimated. Compared with the atmospheric model, these anomalies are all underestimated in the coupled model, which may be related to the ENSO-related SST bias appearing in the Eastern Indian Ocean. Due to the ENSO and ITCZ bias in the historical simulations, the simulated ENSO-related SST and the precipitation anomaly are too equator-trapped in comparison with the observations, and the cold tongue overly extends westward. This limits the ability of the model to simulate ENSO-related EASM variability. For the subseasonal simulations, though atmospheric model simulations can reproduce the westward extension of the Western Pacific subtropic high (WPSH) in EN decaying summers, the eastward retreat of the WPSH in LN is weak. The historical simulations show limited improvement, indicating that the subseasonal variation in the EASM is still a considerable challenge for current generation models." @default.
- W4283274265 created "2022-06-23" @default.
- W4283274265 creator A5009078729 @default.
- W4283274265 creator A5009853448 @default.
- W4283274265 creator A5023043283 @default.
- W4283274265 creator A5064323494 @default.
- W4283274265 creator A5071126099 @default.
- W4283274265 creator A5078949281 @default.
- W4283274265 date "2022-06-21" @default.
- W4283274265 modified "2023-10-06" @default.
- W4283274265 title "Comparison of East Asian Summer Monsoon Simulation between an Atmospheric Model and a Coupled Model: An Example from CAS-ESM" @default.
- W4283274265 cites W1557070555 @default.
- W4283274265 cites W1610718871 @default.
- W4283274265 cites W1974468869 @default.
- W4283274265 cites W1989668498 @default.
- W4283274265 cites W2014570913 @default.
- W4283274265 cites W2019255172 @default.
- W4283274265 cites W2022548072 @default.
- W4283274265 cites W2025306789 @default.
- W4283274265 cites W2030797143 @default.
- W4283274265 cites W2031539993 @default.
- W4283274265 cites W2033990175 @default.
- W4283274265 cites W2046693289 @default.
- W4283274265 cites W2054859717 @default.
- W4283274265 cites W2067141648 @default.
- W4283274265 cites W2070580049 @default.
- W4283274265 cites W2099402228 @default.
- W4283274265 cites W2103492366 @default.
- W4283274265 cites W2103966682 @default.
- W4283274265 cites W2108527489 @default.
- W4283274265 cites W2125073495 @default.
- W4283274265 cites W2131727821 @default.
- W4283274265 cites W2150046129 @default.
- W4283274265 cites W2173049227 @default.
- W4283274265 cites W2181452960 @default.
- W4283274265 cites W2226560196 @default.
- W4283274265 cites W2316283526 @default.
- W4283274265 cites W2317768307 @default.
- W4283274265 cites W2338046588 @default.
- W4283274265 cites W2404021204 @default.
- W4283274265 cites W2460696518 @default.
- W4283274265 cites W2560712914 @default.
- W4283274265 cites W2567966283 @default.
- W4283274265 cites W2594100653 @default.
- W4283274265 cites W2738516213 @default.
- W4283274265 cites W2772535146 @default.
- W4283274265 cites W2788160075 @default.
- W4283274265 cites W2897627506 @default.
- W4283274265 cites W2984603731 @default.
- W4283274265 cites W3004875986 @default.
- W4283274265 cites W3044550370 @default.
- W4283274265 cites W3094301880 @default.
- W4283274265 cites W3096378433 @default.
- W4283274265 cites W3108398410 @default.
- W4283274265 cites W3128887354 @default.
- W4283274265 cites W3165483070 @default.
- W4283274265 cites W414022885 @default.
- W4283274265 cites W4226279930 @default.
- W4283274265 cites W4237401022 @default.
- W4283274265 doi "https://doi.org/10.3390/atmos13070998" @default.
- W4283274265 hasPublicationYear "2022" @default.
- W4283274265 type Work @default.
- W4283274265 citedByCount "1" @default.
- W4283274265 countsByYear W42832742652023 @default.
- W4283274265 crossrefType "journal-article" @default.
- W4283274265 hasAuthorship W4283274265A5009078729 @default.
- W4283274265 hasAuthorship W4283274265A5009853448 @default.
- W4283274265 hasAuthorship W4283274265A5023043283 @default.
- W4283274265 hasAuthorship W4283274265A5064323494 @default.
- W4283274265 hasAuthorship W4283274265A5071126099 @default.
- W4283274265 hasAuthorship W4283274265A5078949281 @default.
- W4283274265 hasBestOaLocation W42832742651 @default.
- W4283274265 hasConcept C107054158 @default.
- W4283274265 hasConcept C111368507 @default.
- W4283274265 hasConcept C118365302 @default.
- W4283274265 hasConcept C121332964 @default.
- W4283274265 hasConcept C122523270 @default.
- W4283274265 hasConcept C127313418 @default.
- W4283274265 hasConcept C12980444 @default.
- W4283274265 hasConcept C12997251 @default.
- W4283274265 hasConcept C132651083 @default.
- W4283274265 hasConcept C13280743 @default.
- W4283274265 hasConcept C134097258 @default.
- W4283274265 hasConcept C136996986 @default.
- W4283274265 hasConcept C150284090 @default.
- W4283274265 hasConcept C153294291 @default.
- W4283274265 hasConcept C166957645 @default.
- W4283274265 hasConcept C168754636 @default.
- W4283274265 hasConcept C191935318 @default.
- W4283274265 hasConcept C205649164 @default.
- W4283274265 hasConcept C23095489 @default.
- W4283274265 hasConcept C26873012 @default.
- W4283274265 hasConcept C2777864850 @default.
- W4283274265 hasConcept C39432304 @default.
- W4283274265 hasConcept C41008148 @default.
- W4283274265 hasConcept C42935608 @default.
- W4283274265 hasConcept C49204034 @default.
- W4283274265 hasConcept C67320510 @default.