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Dust storm observations in Mongolia in spring 2004

机译:2004年春季在蒙古的沙尘暴观测

摘要

[ABSTRACT] A study on dust storms observed over the territory of Mongolia from January to May in 2004 was carried out. Asian regional and local weather maps at surface and 500-hPa level, and NOAA satellite images were used for the study. The study focused on formation, intensity and movement of dust events originated in Mongolian Gobi Desert area. Atmospheric circulation factors causing formation of dust events are reviewed. During the spring, there were 10 cases of strong dust events and 6 moderate or weak dust events in Mongolia. About 6 of them arrived at and Japan via NE China and the Korean Peninsular. Favourable and unfavourable conditions including winter and spring snowfall for the formation of intense dust storms were studied. Snowfall amount was 1- 12 mm over the Gobi Desert area from January to February, and there was no snowfall over the some areas of the Gobi Desert in those months. Monthly precipitation amount in January and February fluctuated around the climate normal between 1961 and 1990, and less than that. March and April of 2004 were the driest months in Mongolia including the Gobi Desert areas. Monthly precipitation amounts were about 0-5 mm over the most areas of Mongolia in those months. Monthly precipitation amounts were less than the climate normal over the Gobi Desert area in Mongolia in the period from March to May. Soil wet was small in winter and spring, and it was favourable for the formation of dust storms in those periods. NOAA satellite images discover dust clouds over NE Asia in spring.
机译:[摘要]对2004年1月至5月在蒙古境内观测到的沙尘暴进行了研究。该研究使用了地表和500-hPa水平的亚洲区域和当地天气图以及NOAA卫星图像。该研究集中于起源于蒙古戈壁沙漠地区的尘埃事件的形成,强度和运动。综述了引起粉尘事件形成的大气循环因素。春季,蒙古有10起强尘事件和6起中度或弱尘事件。其中约有6人经东北中国和朝鲜半岛抵达日本。研究了形成强烈沙尘暴的冬季和春季降雪等有利和不利条件。从一月到二月,戈壁沙漠地区降雪量为1至12毫米,而在那几个月中,戈壁沙漠的某些地区没有降雪。 1961年至1990年期间,1月和2月的月降水量在气候正常范围内波动,并且低于该水平。 2004年3月和4月是蒙古包括戈壁沙漠地区最干旱的月份。在那几个月内,蒙古大部分地区的月降水量约为0-5毫米。在3月至5月期间,蒙古的戈壁沙漠地区每月降水量少于正常的气候。冬春两季土壤湿润小,有利于这段时期形成沙尘暴。 NOAA卫星图像在春季发现了亚洲东北部的尘埃云。

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