Increased air temperatures during the 2010 growing season contributed to an increase in water temperatures. This was reflected in changes in the physicochemical characteristics in the water of the Ild River mouth area, a tributary of the Rybinsk reservoir. During the period of maximum water heating in 2010, the total amount of organic matter, its labile fraction, and suspended solids were significantly higher compared to the period close to the long-term average. Organic matter was predominantly freshly formed compounds; the suspended form of iron predominated over the dissolved one. A highly significant correlation was noted between temperature and organic matter parameters. At the same time, temperature anomalies did not affect the content of dissolved oxygen, mineralization, and color of the water.

2010 年生长季节气温升高导致水温升高。这反映在雷宾斯克水库支流伊尔德河口地区水体物理化学特征的变化上。2010年最大水加热期间，有机物总量、不稳定部分和悬浮物均显着高于接近长期平均水平的时期。有机物主要是新形成的化合物；悬浮形式的铁比溶解形式的铁占主导地位。温度和有机质参数之间存在高度显着的相关性。同时，温度异常并没有影响水体的溶解氧含量、矿化度和颜色。