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Precipitation in the Lake Baikal basin associated with different patterns of atmospheric blocking over Western Siberia

机译:贝加尔湖盆地中的降水与西西伯利亚西西伯利亚的不同大气封闭模式相关

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Since 1996, a low-water period has been observed in the Lake Baikal basin. The decrease of inflow to Lake Baikal isrelated to reduce of the summer discharge of the Selenga River, whose basin makes 83.4% of Lake Baikal catchmentarea. The decrease of river discharge is mainly due to a decrease of midsummer precipitations over the basin that occurs,preferentially, when the frontal system of the East Asian summer monsoon weakens. Some authors suggested that thereason for the East Asian summer monsoon variations is the features of atmospheric circulation at the mid- and highlatitudes of Eurasia. In particular, atmospheric blockings can play an important role.We previously showed the features of formation of July rainfall in the Selenga River basin in different positions ofblocking over Eurasia. We showed that precipitation tends to fall out in Mongolian part of the river basin when blockingis displaced from Western Siberia (WS) to Eastern Siberia (ES). Blocking in these cases may have a dipole configurationwith anticyclonic part over Eastern Siberia and cyclonic part over Mongolia.In this work we continue to study blockings over Siberia and their relations with precipitation in the Selenga Riverbasin in July. As a result we have formulated the following summaries regarding the relationship of WS-blocking andprecipitation in the Selenga basin.1. The maximum amount of precipitation is possible in case of complete blocking offset from West to East Siberiaand formation of blocking over the eastern Siberia.2. The amount of precipitation is not high if the blocking moves from the WS to the ES without formation ofblocking over the eastern Siberia.3. Precipitation in the basin does not fall out in the case of the blocking, which weakly shifts at the end of their lifecycle.4. There is a relationship between lifetime, intensity blocking and its movement over the WS. The stronger theblocking over the WS, the less it moves.
机译:自1996年以来,在贝加尔湖盆地中观察到低水期。贝加尔湖流入的减少是凭借减少SELENGA RIVER的夏季排放,其盆地占贝加尔湖集水区的83.4%区域。河流排放的减少主要是由于盆地上的载体沉淀减少,优先,当东亚夏季季风的正面系统削弱时。一些作者建议东亚夏季季风变异的原因是中高中大气循环的特征欧亚大陆纬度。特别是,大气阻挡可以发挥重要作用。我们此前在不同的位置表明,在Selenga River盆地中形成了7月降雨的特点阻止欧亚大陆。我们表明,在封锁时,降水趋于在河流盆地的蒙古部分脱落从西伯利亚西伯利亚(WS)的流离失所者到西伯利亚东部。在这些情况下阻止可能具有偶极配置在西伯利亚东部的反气旋部分和蒙古的旋风部分。在这项工作中,我们继续研究Selenga河的Sulditation over Siberia和他们的关系盆地7月。因此,我们制定了关于WS阻止的关系的以下摘要Selenga盆地的降水。1.如果从西部到东西伯利亚完全阻止偏移的情况下,可以最大的降水量并在西伯利亚东部封锁的形成。如果阻挡从WS到ES移动而没有形成,则降水量不高阻挡西伯利亚东部。3.盆地中的降水在阻塞的情况下不会脱落,在他们的生命结束时越来越偏移循环。4.在寿命之间,强度阻塞和其在WS上的移动之间存在关系。较强的阻止WS,它移动的越少。

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