During the summer heating, the thermocline conserves the cold intermediate layer (CIL) from above and the halocline converves it from below. The role of the volume absorption of solar irradiance by water and that of the horizontal heat transport increases in the process of the CIL transformation. Surface particles travel around the entire sea transported by the main stream of the Black Sea Rim Current and, on the average, return back after 200 days, while the particles of the CIL cover this distance in four months. Thus, the temperature of the CIL in this stream strongly depends on adection. The order of heat fluxes in the CIL from above q arrow down and below q arrow up is estimated for July. In the deepwater part of the sea, q arrow down = 3.9 X 10~(-5) and q arrow up = 2.4 X 10~9-5) cal/cm~2s. From July to September, the temperature growth in the core of the CIL as 0.5 deg C. Two-thirds of this growth is due to the absorption of solar irraiance and about one-third is due to q arrow down + q arrow up. By the end of water heating (September), the CIL temperature in the horizontal direction over the entire sea basin changes by 0.1-0.2 deg C only.
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机译：在夏季供暖期间，温跃层从上方保留冷的中间层（CIL），而盐环层从下方收敛。在CIL转换过程中，水对太阳辐射的体积吸收和水平热传输的作用增加。黑粒子沿黑海潮流主流运输的整个海洋，并平均在200天后返回，而CIL的粒子在四个月内覆盖了这个距离。因此，该物流中CIL的温度强烈依赖于沉积。估计7月份CIL中从上方q箭头向下和下方q箭头向上的热通量顺序。在海的深水部分，向下的q箭头= 3.9 X 10〜（-5），向上的q箭头= 2.4 X 10〜9-5）cal / cm〜2s。从7月到9月，CIL核心的温度增长为0.5摄氏度。这种增长的三分之二是由于太阳辐射的吸收，而大约三分之一是由于q箭头向下+ q箭头向上。到9月水加热结束时，整个海盆在水平方向上的CIL温度仅变化0.1-0.2摄氏度。
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