Twenty Nile Rivers escape the Mediterranean Sea – a giant water vapor spill boosting the July 2021 floods in Western Europe

Hong-quan Zhang
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Abstract

In summer 2021, severe drought and heatwaves hit the Western United States, Canada, and many other areas around the world. At the same time, record-breaking floods devastated Western Europe (WE) and Central China. Drought and flooding are a water imbalance problem, and heatwaves are always coupled with drought or originate from hot, arid areas. Global average evaporation and precipitation are balanced and steady. When some areas receive less precipitation, other areas receive more, often as heavy downpours. This study analyses one particular freshwater imbalance area – the Mediterranean Basin (MB), from a historical view and of recent trends. The net water vapor output from MB is equivalent to about 20 times the Nile River discharge. The north-south seesaw precipitation trends across Europe clearly indicate a water vapor transfer from MB to Western and Northern Europe. An upper low-pressure system and abundant water vapor supply from MB are an ideal combination for lingering heavy downpours and floods over WE, such as the case in July 2021. The root cause of MB freshwater imbalance is identified as the Sahara expansion. The breach of the green Sahara about 5700 years ago was the desiccation of the Atlas Basin. Based on water cycle stability a solution is suggested to restore the Sahara back to green.
20条尼罗河从地中海流出,巨大的水汽泄漏加剧了2021年7月西欧的洪水
2021年夏天,严重的干旱和热浪袭击了美国西部、加拿大和世界各地的许多其他地区。与此同时,破纪录的洪水摧毁了西欧和中国中部。干旱和洪水是一个水资源不平衡的问题,而热浪总是伴随着干旱或起源于炎热干旱的地区。全球平均蒸发和降水是平衡和稳定的。当一些地区降水减少时,其他地区降水增加,通常是倾盆大雨。本研究分析了一个特殊的淡水失衡地区-地中海盆地(MB),从历史的角度和最近的趋势。MB的净水汽输出大约相当于尼罗河流量的20倍。整个欧洲的南北跷跷板降水趋势清楚地表明水汽从欧洲中部向西欧和北欧转移。高空低压系统和来自MB的丰富水汽供应是WE上空持续暴雨和洪水的理想组合,例如2021年7月的情况。撒哈拉扩张是造成撒哈拉沙漠淡水失衡的根本原因。大约5700年前,绿色撒哈拉沙漠的裂口是阿特拉斯盆地的干涸。基于水循环稳定性,提出了撒哈拉沙漠恢复绿色的解决方案。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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