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Evaluation of sea surface temperature and wind speed observed by GCOM-W1/AMSR2 using in situ data and global products

机译:利用GCOM-W1 / AMSR2利用原位数据和全球产品评估海表温度和风速

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The Global Change Observation Mission (GCOM) 1st-Water (GCOM-W1) satellite, equipped with the Advanced Microwave Scanning Radiometer 2 (AMSR2), was launched on May 18, 2012, by the Japan Aerospace Exploration Agency (JAXA), and began observing on July 3, 2012. In this study, we evaluated the sea surface temperature (SST) and sea surface wind speed (SSW) data from the AMSR2 (ver. 1) standard product, provided by JAXA, by comparison with mooring buoy data or global products. From a comparison of the AMSR2 and Triangle Trans-Ocean Buoy Network (TRITON) data, mean differences of 0.21 degrees C and 030 m/s, and root mean square (RMS) differences of 0.49 degrees C and 125 m/s, were inferred for SST and SSW, respectively. During daytime low wind-speed conditions, SSTs from AMSR2 are significantly higher than from TRITON. This implies that SSTs from AMSR2 are strongly affected by diurnal heating. From an intercomparison of global products for the Southern Ocean, the annual-mean SSW from AMSR2 is as much as 1 m/s lower than values from other SSW products. Although the SSW data from AMSR2 have a similar accuracy to data from other products, the AMSR2 data have the advantage of fewer missing data compared with other products. Furthermore, we checked for significant differences in annual means by comparing data from WindSat, AMSR2, and AMSR for the Earth Observing System (AMSR-E) provided by JAXA. For the Southern Ocean, we found remarkable differences in the annual-mean values of SST and SSW. SSTs from AMSR2 are lower than from WindSat in regions of strong current in the Northern Hemisphere, and SSTs from AMSR-E JAXA are higher than from WindSat in the same regions. However, the results also suggest a risk of artificial trends in the satellite data if AMSR2, AMSR-E JAXA, and WindSat data are used continuously. (C) 2015 Elsevier Inc. All rights reserved.
机译:配备有先进微波扫描辐射计2(AMSR2)的全球变化观察团(GCOM)一水(GCOM-W1)卫星由日本航空航天局(JAXA)于2012年5月18日发射,并开始了于2012年7月3日观测到的数据。在本研究中,我们通过与JAXA提供的AMSR2(版本1)标准产品的海面温度(SST)和海面风速(SSW)数据进行了比较,并与系泊浮标数据进行了比较或全球产品。通过对AMSR2和三角跨洋浮标网络(TRITON)数据的比较,推断出0.21摄氏度和030 m / s的均方差以及0.49摄氏度和125 m / s的均方根(RMS)差异分别用于SST和SSW。在白天低风速条件下,来自AMSR2的SST明显高于来自TRITON的SST。这意味着来自AMSR2的SST受昼夜加热的强烈影响。通过对南大洋全球产品的比较,AMSR2的年平均SSW比其他SSW产品的值低1 m / s。尽管来自AMSR2的SSW数据的准确性与来自其他产品的数据相似,但AMSR2数据的优势在于与其他产品相比丢失的数据更少。此外,我们通过比较来自JAXA提供的WindSat,AMSR2和AMSR的地球观测系统(AMSR-E)数据,检查了年度平均值的显着差异。对于南大洋,我们发现SST和SSW的年均值存在显着差异。在北半球强流区域,来自AMSR2的SST比来自WindSat的低,而在同一地区,来自AMSR-E JAXA的SST高于来自WindSat的SST。但是,结果还表明,如果连续使用AMSR2,AMSR-E JAXA和WindSat数据,则有人造数据趋势的风险。 (C)2015 Elsevier Inc.保留所有权利。

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