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首页> 外文期刊>Journal of Geophysical Research, C. Oceans: JGR >Evaluation of a hybrid satellite- and NWP-based turbulent heat flux product using Tropical Atmosphere-Ocean (TAO) buoys
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Evaluation of a hybrid satellite- and NWP-based turbulent heat flux product using Tropical Atmosphere-Ocean (TAO) buoys

机译:使用热带大气-海洋(TAO)浮标评估基于卫星和基于NWP的混合湍流通量产品

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Gridded hybrid turbulent heat flux fields were created by applying the state-of-the-art Coupled Ocean-Atmosphere Response Experiment (COARE) version 3.0 bulk algorithm to state variables (sea surface temperature, winds relative to currents, air temperature, and air specific humidity) derived from either numerical weather prediction (NWP) reanalysis (National Centers for Environmental Prediction–National Center for Atmospheric Research (NCEP-NCAR) reanalysis (NCEP1), NCEP reanalysis-2 (NCEP2), and 40-year European Centre for Medium-Range Weather Forecasts (ECMWF) reanalysis (ERA40)) or satellite sensors (QuikSCAT winds and Tropical Rainfall Measuring Mission (TRMM) Microwave Imager microwave sea surface temperature). The most accurate source for each state variable was determined by comparing variables to tropical Pacific Tropical Atmosphere-Ocean (TAO) buoy observations for the years 2000–2001. The selected sources were as follows: QuikSCAT for winds relative to currents, ERA40 for air temperature and specific humidity, and TRMM Microwave Imager fusion product for sea surface temperature. Errors in latent and sensible heat fluxes to state variables were analyzed. Specific humidity errors contributed the most to errors in latent heat flux (LHF). Overall, the hybrid LHF product had a bias of ?5.8 W m?2 and a standard deviation of difference of 16.2 W m?2, which is comparable to the accuracy of LHF derived from TAO measurements.
机译:通过将最新的耦合海洋-大气响应实验(COARE)3.0版体积算法应用于状态变量(海表温度,相对于洋流的风,空气温度和特定于空气的温度),创建了网格混合湍流热通量场。湿度)来自数值天气预报(NWP)重新分析(国家环境预测中心-国家大气研究中心(NCEP-NCAR)重新分析(NCEP1),NCEP reanalysis-2(NCEP2)和40年的欧洲中等水平研究中心-范围天气预报(ECMWF)重新分析(ERA40))或卫星传感器(QuikSCAT风和热带降雨测量任务(TRMM)微波成像仪微波海面温度)。通过将变量与2000-2001年的热带太平洋热带大气-海洋(TAO)浮标观测值进行比较,可以确定每个状态变量的最准确来源。选择的来源如下:QuikSCAT用于相对于风的风,ERA40用于气温和比湿,以及TRMM Microwave Imager融合产品用于海面温度。分析了状态变量的潜热通量和显热通量的误差。特定的湿度误差对潜热通量(LHF)的误差影响最大。总体而言,混合LHF产品的偏差为5.8 W m 2,标准差为16.2 W m 2,与从TAO测量得出的LHF精度相当。

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