首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >Pacific Ocean wind stress and surface heat flux anomalies from NCEP reanalysis and observations: Cross-statistics and ocean model responses
【24h】

Pacific Ocean wind stress and surface heat flux anomalies from NCEP reanalysis and observations: Cross-statistics and ocean model responses

机译:来自NCEP重新分析和观测的太平洋风应力和表面热通量异常:交叉统计和海洋模型响应

获取原文
获取原文并翻译 | 示例
           

摘要

Wind stresses and surface heat fluxes over the Pacific Ocean from the National Center for Environmental Prediction (NCEP) reanalysis and the comprehensive Ocean-Atmosphere Data Set (COADS) (blended with FSU tropical wind stresses) are compared over a common time interval (1958-1997) in their statistics anal in the responses that they induce in sea surface temperature (SST) and heat storage when used to force an ocean model. Wind stress anomalies from the two data sets are well correlated in the midlatitude extratropics, especially in the highly sampled North Pacific. In the tropics and subtropics, low correlations were found between the two wind stress data sets. The amplitudes of the stress variations of the two data sets are similar in midlatitudes, but in the tropics NCEP wind stresses are weaker than the LOADS/FSU stresses, especially on interannual timescales. Surface heat flux anomalies from the two data sets are well correlated on interannual and shorter timescales in the North Pacific Ocean poleward of 20 degreesN, but they are poorly correlated elsewhere and on decadal timescales. In the extratropics the amplitudes of the heat flux variations of the two data sets are comparable, but in the tropics the NCEP heat fluxes are weaker than those of CORDS. Ocean model hindcasts driven by bath data sets are also compared: The midlatitude SST hindcasts were superior when using the NCEP flux anomalies while tropical SST hindcasts were equally skillful for the two hindcasts when considering all climatic timescales. The spatial and temporal sampling rates of the LOADS observations and their consequent impacts on constraining the NCEP reanalysis appear to be the main factors controlling the results found here. [References: 75]
机译:比较了美国国家环境预测中心(NCEP)重新分析和整个海洋大气数据集(COADS)(与FSU热带风应力混合而成)在太平洋上的风应力和表面热通量(在1958- (1997年)在他们的统计资料中分析了他们在强迫海洋模型时在海表温度(SST)和储热中引起的响应。来自这两个数据集的风应力异常在中纬度热带特别是高度相关,特别是在高度采样的北太平洋。在热带和亚热带,两个风应力数据集之间的相关性较低。这两个数据集的应力变化幅度在中纬度上相似,但在热带地区,NCEP的风应力比LOADS / FSU应力弱,尤其是在年际时标上。来自两个数据集的表面热通量异常在北太平洋极向20°N的年际和较短的时间尺度上具有很好的相关性,但在其他地方和年代际尺度上却没有很好的相关性。在热带地区,两个数据集的热通量变化幅度是可比较的,但是在热带地区,NCEP热通量比CORDS的弱。还比较了由浴场数据集驱动的海洋模型后兆:当使用NCEP通量异常时,中纬度SST后兆要好,而考虑所有气候时间尺度时,热带SST后兆对于这两个后兆同样熟练。 LOADS观测值的时空采样率及其对约束NCEP重新分析的影响似乎是控制此处结果的主要因素。 [参考:75]

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号