冬季白令海上层混合层热态的年际变化

V. A. Luchin
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引用次数: 0

摘要

利用迄今为止可获得的所有深海海洋学观测数据(1943年至2022年期间12430个站点),研究了白令海无冰水域在寒冷季节(12月至3月)上层混合层温度的年际变化。利用经验正交函数(EOF)对12 - 3月混合层温度年平均场序列进行分解;分析了分解的前两个分量(合计占初始场变率的50.4%)的动力学。第一个分量(占变化量的32.4%)表明整个海域的同步振荡,其中大陆坡的贡献最大。第二个分量(18.0%的方差)反映了位于从纳瓦林角到阿拉斯加半岛的大陆斜坡以及深盆地的西部、中部和南部的两个广阔海域的相反振荡。波谱分析显示,第一次EOF和准两年周期为4年、7年和17-20年,第二次EOF的周期为3年和4年。第一次EOF的时间系数在1958-2022年期间呈显著的线性增温趋势。用6度多项式函数逼近该系数动态(多项式趋势)表明,1969-1972年和1992-2004年冬季混合层有变冷的趋势,而1973-1991年和2005-2022年冬季则相反。第2次EOF时间系数的变化趋势与第2次EOF正值和负值区域相反。1958 - 2022年期间,白令海的冬季仅考虑第一次EOF的贡献,根据混合层温度分类为“温暖”(1958、1959、1963、1964、1966、1979、1982、1985、1987、1997、2001、2003、2004、2015-2018、2020和2022)、“正常”(1960-1962、1965、1967、1968、1970、1971、1974、1978、1980、1981、1983、1986、1989-1994、1996、1998、2005-2007、2011、2013、2014、2019和2021)、“寒冷”(1969、1972、1973、1975-1977、1984、1988、1995、1999、1999、1998、1998、2011、2013、2014、2019和2021)。2000年、2002年、2008年和2010年),以及极度寒冷(2009年和2012年)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Interannual variability in thermal state of the upper mixed layer in the Bering Sea in winter
Year-to-year variations of temperature in the upper mixed layer are considered for the ice-free waters of the Bering Sea in cold season (from December to March) using all data of the deep-sea oceanographic observations available to date (12,430 stations for the period from 1943 to 2022). Series of annual mean fields of the mixed layer temperature in December-March were decomposed by applying the empirical orthogonal function (EOF); dynamics of the first two components of decomposition (described in sum 50.4 % of the initial fields variability) are analyzed. The first component (32.4 % of variation) indicates synchronous oscillations over the entire sea area with the maximum contribution at the continental slope. The second component (18.0 % of variance) reflects opposite oscillations in two vast regions of the sea located along the continental slope from Cape Navarin to Alaska Peninsula and in the western, central and southern parts of the deep basin. The following statistically significant periodic oscillations are revealed by spectral analysis: quasi-biennial and those with periods of 4, 7, and 17–20 year for the 1st EOF and quasi-biennial and those with periods of 3 and 4 year for the 2nd EOF. A statistically significant linear trend to warming is detected for the time coefficient of the 1st EOF in the period of 1958–2022. Approximation of this coefficient dynamics with 6-degree polynomial function (polynomial trend) shows a tendencies to the mixed layer cooling in winters of 1969–1972 and 1992–2004 but the opposite tendencies to warming in 1973–1991 and 2005–2022. Variations of time coefficient for the 2nd EOF correspond to opposite tendencies in the areas with positive and negative values of this EOF. For the period from 1958 to 2022, winters in the Bering Sea are classified by the mixed layer temperature, taking into account the contribution of the 1st EOF only, as «warm» (1958, 1959, 1963, 1964, 1966, 1979, 1982, 1985, 1987, 1997, 2001, 2003, 2004, 2015–2018, 2020, and 2022), «normal» (1960–1962, 1965, 1967, 1968, 1970, 1971, 1974, 1978, 1980, 1981, 1983, 1986, 1989–1994, 1996, 1998, 2005–2007, 2011, 2013, 2014, 2019, and 2021), «cold» (1969, 1972, 1973, 1975–1977, 1984, 1988, 1995, 1999, 2000, 2002, 2008, and 2010), and extremely cold (2009 and 2012).
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