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首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >INTERANNUAL VARIATIONS IN ANTARCTIC PRECIPITATION RELATED TO EL NINO SOUTHERN OSCILLATION
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INTERANNUAL VARIATIONS IN ANTARCTIC PRECIPITATION RELATED TO EL NINO SOUTHERN OSCILLATION

机译:与厄尔尼诺南方涛动有关的南极降水年际变化

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摘要

The accurate estimation of Antarctic precipitation variability is an essential component in understanding global sea level fluctuations; direct measurement techniques, however, are replete with practical difficulties. In this study, net precipitation (precipitation minus sublimation) for the Antarctic continent is computed for 1980-1994 using operational numerical analyses obtained from the ECMWF (European Centre for Medium-Range Weather Forecasts). The resulting estimations reveal a strong interannual variability for the Antarctic continent, implying a +/-1.2 - 1.5 mm yr(-1) maximum range in the Antarctic eustatic change contribution. In particular, variability for the South Pacific sector (120 degrees W-180 degrees W) is shown to be correlated with the El Nino-Southern Oscillation (ENSO) phenomenon for 1980-1990. The relation becomes anticorrelated after 1990, associated with a strong East Antarctic ridging pattern that coincides with the start of the prolonged series of warm events of the early 1990s. This result is relevant to other studies relating ENSO variability to high southern latitudes, and a more elaborate picture of this teleconnection pattern is presented. Comparisons of sea level pressure values using available ship observations show good agreement and offer a confirmation of the analyses in this data-sparse region. Additionally, a comparison of results with values obtained from the precipitation fields of the NCEP/NCAR (NCEP: National Centers for Environmental Prediction; NCAR: National Center for Atmospheric Research) reanalysis project are discussed. [References: 67]
机译:准确估算南极降水变化是了解全球海平面波动的重要组成部分;然而,直接测量技术充满了实际困难。在这项研究中,使用从ECMWF(欧洲中距离天气预报中心)获得的运营数值分析计算了1980-1994年南极大陆的净降水量(降水减去升华)。由此得出的估计值揭示了南极大陆的强烈年际变化,这意味着南极洲的欣喜变化贡献最大范围为+/- 1.2-1.5 mm yr(-1)。特别是,南太平洋地区的变率(120度W-180度W)与1980-1990年的厄尔尼诺-南方涛动(ENSO)现象相关。 1990年以后,这种关系变得反相关,伴随着强烈的南极东部褶皱格局,这与1990年代初一系列长期暖事件的开始相吻合。该结果与其他有关ENSO变异性与南部高纬度的研究有关,并且对该遥距模式进行了更为详尽的描述。使用现有的船舶观测值比较海平面压力值显示出很好的一致性,并为该数据稀疏区域的分析提供了确认。此外,还讨论了结果与从NCEP / NCAR(NCEP:国家环境预测中心; NCAR:国家大气研究中心)再分析项目的降水场获得的值的比较。 [参考:67]

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