The distribution of desalinated waters from the Amur Estuary in the northwestern Sea of Okhotsk during the summer period is analyzed using satellite data on the sea surface height (SSH), sea surface salinity (SSS), temperature, and concentrations of particulate organic carbon. There is a good agreement between the spatial distributions of SSS (data from the SMAP satellite) and SSH (AVISO data) in the study area. Identification of the Amur Estuary waters in terms of surface water temperature and concentration of particulate organic carbon is confined by Sakhalin Bay and the coastal zone of Sakhalin Island. An increase (a decrease) in the Amur River discharge during the spring–summer high-water period leads to an increase (a decrease) in the SSH in the northern part of Sakhalin Bay in July. Strengthening of the northwestern (southeastern) winds in September reduces (increases) the inflow of waters with low salinity and causes an elevated SSH in the water area to the north of Sakhalin Bay.

中文翻译：

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鄂霍次克海阿穆尔河口淡化水体卫星观测分布

使用有关海面高度 (SSH)、海面盐度 (SSS)、温度和颗粒有机碳浓度的卫星数据分析了夏季期间鄂霍次克海西北部阿穆尔河口淡化海水的分布情况。研究区SSS（SMAP卫星数据）和SSH（AVISO数据）空间分布具有较好的一致性。根据地表水温和颗粒有机碳浓度对阿穆尔河口水域的识别受萨哈林湾和萨哈林岛沿海地区的限制。春夏高水期阿穆尔河流量增加（减少）导致库页岛北部 7 月 SSH 增加（减少）。