Wentz Frank J, Ricciardulli Lucrezia, Rodriguez Ernesto, Stiles Bryan W, Bourassa Mark A, Long David G, Hoffman Ross N, Stoffelen Ad, Verhoef Anton, O'Neill Larry W, Farrar J Tomas, Vandemark Douglas, Fore Alexander G, Hristova-Veleva Svetla M, Turk F Joseph, Gaston Robert, Tyler Douglas
Remote Sensing Systems, Santa Rosa, CA 95401 USA.
Jet Propulsion Laboratory, Pasadena, CA 91109 USA.
IEEE J Sel Top Appl Earth Obs Remote Sens. 2017 May;10(5):2165-2185. doi: 10.1109/JSTARS.2016.2643641. Epub 2017 May 23.
Satellite microwave sensors, both active scatterometers and passive radiometers, have been systematically measuring near-surface ocean winds for nearly 40 years, establishing an important legacy in studying and monitoring weather and climate variability. As an aid to such activities, the various wind datasets are being intercalibrated and merged into consistent climate data records (CDRs). The ocean wind CDRs (OW-CDRs) are evaluated by comparisons with ocean buoys and intercomparisons among the different satellite sensors and among the different data providers. Extending the OW-CDR into the future requires exploiting all available datasets, such as OSCAT-2 scheduled to launch in July 2016. Three planned methods of calibrating the OSCAT-2 measurements include 1) direct Ku-band intercalibration to QuikSCAT and RapidScat; 2) multisensor wind speed intercalibration; and 3) calibration to stable rainforest targets. Unfortunately, RapidScat failed in August 2016 and cannot be used to directly calibrate OSCAT-2. A particular future continuity concern is the absence of scheduled new or continuation radiometer missions capable of measuring wind speed. Specialized model assimilations provide 30-year long high temporal/spatial resolution wind vector grids that composite the satellite wind information from OW-CDRs of multiple satellites viewing the Earth at different local times.
卫星微波传感器,包括有源散射计和无源辐射计,已经系统地测量近地表海洋风近40年了,在研究和监测天气及气候变率方面留下了重要遗产。作为此类活动的辅助手段,各种风数据集正在进行相互校准,并合并成一致的气候数据记录(CDR)。通过与海洋浮标进行比较以及在不同卫星传感器之间和不同数据提供者之间进行相互比较,对海洋风CDR(OW-CDR)进行评估。将OW-CDR扩展到未来需要利用所有可用数据集,例如计划于2016年7月发射的OSCAT-2。校准OSCAT-2测量的三种计划方法包括:1)直接将Ku波段与QuikSCAT和RapidScat进行相互校准;2)多传感器风速相互校准;3)校准到稳定的雨林目标。不幸的是,RapidScat于2016年8月出现故障,无法用于直接校准OSCAT-2。未来一个特别令人担忧的连续性问题是,没有计划中的能够测量风速的新的或延续性辐射计任务。专门的模型同化提供了长达30年的高时空分辨率风矢量网格,这些网格综合了来自多颗在不同当地时间观测地球的卫星的OW-CDR中的卫星风信息。