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OBSERVATIONS OF DUST-STORMS IN CHINA,MONGOLIA AND ASSOCIATED DUST FALLS IN KOREA IN SPRING 2003

机译:2003年春季中国,蒙古和韩国相关的沙尘暴观测

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A joint monitoring of dust-storms that occurred in East Asia from March until May 2003 has been carried.Our discussions include dust-storm observations in the source areas of China and Mongolia,and measurements with satellites and ground monitors in central Korea.Differences were found in the definition and measurement of dust-storms.Over the source area of Mongolia there were 6 dusty days in March,18 days in April,and 10 dusty days in May.In Inner Mongolia of northern China there were 4 dust-storms with 14 dusty days observed over the three months.In central Korea,a sink area,there were 4 cases of weak dust-storm and 17 dusty days in the spring of 2003.The highest PM10 value was 607 mugm~(-3) and PM 2.3 was 149 mugm~(-3),respectively.These observations identify the growing need for further universal observation practices and dust-storm reporting in future. Observations indicated that snow covered the central part of the Gobi Desert,near the boundary of China and Mongolia,from December until mid-March.This is in contrast to other years when the Gobi was relatively wet,producing unfavourable conditions for the formation of intense dust-storms.In addition,the very strong winds associated with intense cyclones and anticyclones were not apparent and the systems shifted northward during the spring.As a result,the frequency and intensity of observed dust-storms in 2003 in this region were very low.This confirms that there is variability in the frequency of dust-storm formation due to the current process of desertification and climate change.
机译:开展了对2003年3月至2003年5月在东亚发生的沙尘暴的联合监测。我们的讨论包括在中国和蒙古的源区进行沙尘暴观测以及在朝鲜中部使用卫星和地面监测仪进行测量。在沙尘暴的定义和测量中发现。在蒙古源地区,3月有6个沙尘暴天,4月有18天,5月有10个沙尘暴天。中国北方的内蒙古有4个沙尘暴,在过去的三个月中观察到14个尘土飞扬的日子。在朝鲜中部的一个水槽地区,2003年春季有4例微弱的沙尘暴和17个尘土飞扬的日子。最高PM10值为607 mugm〜(-3)和PM 2.3分别为149 mugm〜(-3)。这些观测结果表明,将来对进一步的通用观测方法和沙尘暴报告的需求正在增长。观测表明,从12月到3月中旬,积雪覆盖了中蒙边界附近的戈壁沙漠中心地区,这与戈壁相对较湿的其他年份形成强烈的形成不利条件形成了鲜明对比。此外,与强旋风和反旋风相关的强风并不明显,并且系统在春季期间向北移动。结果,该地区2003年观测到的沙尘暴的频率和强度都非常低。这证实了由于当前沙漠化和气候变化的过程,沙尘暴形成的频率存在差异。

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