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首页> 外文期刊>Journal of Geophysical Research, C. Oceans: JGR >Satellite-derived variability in chlorophyll, wind stress, sea surface height, and temperature in the northern California Current System
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Satellite-derived variability in chlorophyll, wind stress, sea surface height, and temperature in the northern California Current System

机译:卫星衍生的北加州洋流系统中的叶绿素,风应力,海面高度和温度的变化

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Satellite-derived data provide the temporal means and seasonal and nonseasonal variability of four physical and biological parameters off Oregon and Washington (41°–48.5°N). Eight years of data (1998–2005) are available for surface chlorophyll concentrations, sea surface temperature (SST), and sea surface height, while six years of data (2000–2005) are available for surface wind stress. Strong cross-shelf and alongshore variability is apparent in the temporal mean and seasonal climatology of all four variables. Two latitudinal regions are identified and separated at 44°–46°N, where the coastal ocean experiences a change in the direction of the mean alongshore wind stress, is influenced by topographic features, and has differing exposure to the Columbia River Plume. All these factors may play a part in defining the distinct regimes in the northern and southern regions. Nonseasonal signals account for ~60–75% of the dynamical variables. An empirical orthogonal function analysis shows stronger intra-annual variability for alongshore wind, coastal SST, and surface chlorophyll, with stronger interannual variability for surface height. Interannual variability can be caused by distant forcing from equatorial and basin-scale changes in circulation, or by more localized changes in regional winds, all of which can be found in the time series. Correlations are mostly as expected for upwelling systems on intra-annual timescales. Correlations of the interannual timescales are complicated by residual quasi-annual signals created by changes in the timing and strength of the seasonal cycles. Examination of the interannual time series, however, provides a convincing picture of the covariability of chlorophyll, surface temperature, and surface height, with some evidence of regional wind forcing.
机译:卫星数据提供了俄勒冈和华盛顿(41°–48.5°N)附近四个物理和生物学参数的时间均值以及季节性和非季节性的变化。可获得八年的数据(1998-2005年)用于表层叶绿素浓度,海表温度(SST)和海面高度,而可获得六年的数据(2000-2005年)用于表层风应力。在所有四个变量的时间平均和季节气候学中,很明显的跨架和沿海变化。确定了两个纬度区域,并在44°-46°N处分开,其中沿海海洋沿平均沿海风应力方向发生变化,受地形特征影响,并且对哥伦比亚河羽的暴露程度不同。所有这些因素都可能在定义北部和南部地区不同的政权方面发挥作用。非季节信号占动态变量的60〜75%。经验正交函数分析显示,沿岸风,沿海海温和表层叶绿素的年际变化较大,而表层高度的年际变化较大。年际变化可能是由于距赤道和盆地尺度的环流变化的远距离强迫,或者是区域风的更局限性变化造成的,所有这些都可以在时间序列中找到。在年内时间尺度上,相关性大多数与上升流系统的预期一样。年际时间尺度的相关性由于季节周期的时间和强度的变化而产生的残留准年信号而变得复杂。然而,对年际时间序列的检验提供了令人信服的画面,显示了叶绿素,表面温度和表面高度的协变性,并有区域风强迫的证据。

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