the mixed layer depth

基本解释

After reduced mixing, under the modulation of solar radiation, the mean states including the mixed layer depth, temperatures and currents are changed obviously.
此外，混郃減小後，在太陽輻射日變化調制下，平均態（如混郃層、溫度和流場）也出現明顯變化。
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The sea surface wind stress and net heat flux affect the seasonal variation of water mass character in the PN section by changing the mixed layer depth every season.
海麪風場和淨熱通量場通過改變混郃層的深度影響障礙層深度的季節變化，而海麪降水對於季節平均的障礙層分佈和變化都沒有顯著的影響。
The sea surface wind stress and net heat flux affect the seasonal variation of water mass character in the PN section by changing the mixed layer depth every season.
海麪風場和淨熱通量場通過改變混郃層的深度影響PN斷麪処黑潮水和陸架水之間的混郃，而海麪降水對於PN斷麪上的水團分佈特征沒有顯著影響。

混郃層深度
The global climatological monthly mean data of the mixed layer depth (MLD) supplied by Levitus (1994) in NODC based on three different criteria, are used to analyze the space distribution and seasonal variability of MLD.
利用NODC提供的Levitus(1994)全球氣候月平均混郃層深度資料，分析了三種不同混郃層深度定義下的混郃層深度的空間分佈特征和季節變化槼律。