FN Archimer Export Format PT J TI Uncertainties in Ocean Latent Heat Flux Variations over Recent Decades in Satellite-Based Estimates and Reduced Observation Reanalyses BT AF Robertson, Franklin R. Roberts, Jason B. Bosilovich, Michael G. Bentamy, Abderrahim Clayson, Carol Anne Fennig, Karsten Schröder, Marc Tomita, Hiroyuki Compo, Gilbert P. Gutenstein, Marloes Hersbach, Hans Kobayashi, Chiaki Ricciardulli, Lucrezia Sardeshmukh, Prashant Slivinski, Laura C. AS 1:1;2:1;3:2;4:3;5:4;6:5;7:5;8:6;9:7,8;10:5;11:9;12:10;13:11;14:7,8;15:7,8; FF 1:;2:;3:;4:PDG-ODE-LOPS-SIAM;5:;6:;7:;8:;9:;10:;11:;12:;13:;14:;15:; C1 NASA Marshall Space Flight Center, Huntsville, Alabama NASA GSFC Global Modeling and Assimilation Office, Greenbelt, Maryland Laboratoire d’Océanographie Spatiale, Institut Français pour la Recheche et l’Exploitation de la Mer (IFREMER), Brest, France Woods Hole Oceanographic Institution, Woods Hole, Massachusetts Satellite-Based Climate Monitoring, Deutscher Wetterdienst, Offenbach, Germany Institute for Space-Earth Environmental Research, Nagoya University, Nagoya, Japan Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, Colorado NOAA Physical Sciences Laboratory, Boulder, Colorado European Centre for Medium-Range Weather Forecasts, Reading, United Kingdom Meteorological Research Institute, Tsukuba, Japan Remote Sensing Systems, Santa Rosa, California C2 NASA, USA NASA, USA IFREMER, FRANCE WHOI, USA CM SAF, GERMANY UNIV NAGOYA, JAPAN UNIV COLORADO BOULDER, USA NOAA, USA ECMWF, UK METEOROL RES INST, JAPAN REMOTE SENSING SYSTEMS, USA SI BREST SE PDG-ODE-LOPS-SIAM UM LOPS IN WOS Ifremer UMR copubli-europe copubli-int-hors-europe IF 5.148 TC 15 UR https://archimer.ifremer.fr/doc/00654/76588/77737.pdf LA English DT Article AB 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) singlesensor 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. PY 2020 PD OCT SO Journal Of Climate SN 0894-8755 PU American Meteorological Society VL 33 IS 19 UT 000589983000014 BP 8415 EP 8437 DI 10.1175/JCLI-D-19-0954.1 ID 76588 ER EF