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Uncertainties in Ocean Latent Heat Flux Variations over Recent Decades in Satellite-Based Estimates and Reduced Observation Reanalyses

机译:海洋潜热通量的不确定性近几十年来卫星基于卫星的估计和减少观察Reanalyses

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Four state-of-the-art satellite-based estimates of ocean surface latent heat fluxes (LHFs) extending over three decades are analyzed, focusing on the interannual variability and trends of near-global averages and regional patterns. Detailed intercomparisons are made with other datasets including 1) reduced observation reanalyses (RedObs) whose exclusion of satellite data renders them an important independent diagnostic tool; 2) a moisture budget residual LHF estimate using reanalysis moisture transport, atmospheric storage, and satellite precipitation; 3) the ECMWF Reanalysis 5 (ERA5); 4) Remote Sensing Systems (RSS) single-sensor passive microwave and scatterometer wind speed retrievals; and 5) several sea surface temperature (SST) datasets. Large disparities remain in near-global satellite LHF trends and their regional expression over the 1990-2010 period, during which time the interdecadal Pacific oscillation changed sign. The budget residual diagnostics support the smaller RedObs LHF trends. The satellites, ERA5, and RedObs are reasonably consistent in identifying contributions by the 10-m wind speed variations to the LHF trend patterns. However, contributions by the near-surface vertical humidity gradient from satellites and ERA5 trend upward in time with respect to the RedObs ensemble and show less agreement in trend patterns. Problems with wind speed retrievals from Special Sensor Microwave Imager/Sounder satellite sensors, excessive upward trends in trends in Optimal Interpolation Sea Surface Temperature (OISST AVHRR-Only) data used in most satellite LHF estimates, and uncertainties associated with poor satellite coverage before the mid-1990s are noted. Possibly erroneous trends are also identified in ERA5 LHF associated with the onset of scatterometer wind data assimilation in the early 1990s.
机译:分析了四十多年来延伸的四种最先进的基于卫星基于卫星的卫星基于海洋表面潜热通量(LHFS),重点关注近全球平均值和区域模式的年性变异性和趋势。详细的离法比喻由其他数据集进行,包括1)减少观察Reanalyses(Redobs),其排除卫星数据呈现重要的独立诊断工具; 2)使用再分析水分运输,大气储存和卫星沉淀的水分预算残留的LHF估计; 3)ECMWF Reanalysis 5(ERA5); 4)遥感系统(RSS)单传感器无源微波和散射仪风速检索; 5)几个海表面温度(SST)数据集。在1990 - 2010年期间,近全球卫星LHF趋势及其区域表达仍然存在巨大的差异,在此期间,Interdecadal Pacific振荡改变了迹象。预算剩余诊断支持较小的REDOBS LHF趋势。卫星,ERA5和REDOBS在识别LHF趋势模式的10米风速变化的贡献中是合理的一致。然而,通过卫星和ERA5的近表面垂直湿度梯度以及在趋势模式中的趋势较少的时间上向上趋向于卫星和ERA5趋势的贡献。来自特殊传感器微波成像仪/探测器卫星传感器的风速检索问题,最佳插值海面温度(仅限OISST AVHRR-ock)数据的过度向上趋势趋势(OISST AVHRR-ock)数据,以及在中期之前的卫星覆盖率相关的不确定性注意到-1990s。在20世纪90年代初期与散射仪风数据同化发作相关的ERA5 LHF中也识别出可能的错误趋势。

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