After the screening, the number of stations in which 7, 8, and 9 yr of data survived are 8, 37, and 47, respectively. The same twice-daily precipitation are recorded for several consecutive days, and these values are discarded (two cases).

Some outliers naturally remain after this simple quality control check. The stationary Rossby wave was climatologically phase locked in seasonal evolution and the mean amplitude reached a maximum around the middle of July, as the result, the timing of the break in the Mongolian rainy season was also concentrated around the middle of July.This research has been supported by a CREST Project (The Rangelands Atmosphere–Hydrosphere–Biosphere Interaction Study Experiment in Northeastern Asia of the Japan Science and Technology Agency (JST), and partially supported by the Ministry of Education, Sports, Culture, Science, and Technology of Japan.

Large rain drops become increasingly flattened on the bottom, like Rain drops associated with melting hail tend to be larger than other rain drops.Intensity and duration of rainfall are usually inversely related, i.e., high intensity storms are likely to be of short duration and low intensity storms can have a long duration.The final droplet size distribution is an Deviations can occur for small droplets and during different rainfall conditions. Hawaii was the only region to show a decrease (−9.25 percent).Analysis of 65 years of United States of America rainfall records show the lower 48 states have an increase in heavy downpours since 1950. Therefore, most of erroneous values in this dataset are missing values. There has been an increase in the number of heavy precipitation events over many areas during the past century, as well as an increase since the 1970s in the prevalence of droughts—especially in the tropics and subtropics. Arrows indicate the break period for each year.Properties of the break in each rainy season. However, we could not elucidate the difference between Type I and Type II in a meteorological process, and the two types will be treated as the same.Thirty-two and nine stations satisfied the criteria for Type I and Type II breaks, respectively. The arrow indicates the “break” in the Mongolian rainy season.Seasonal change of (a) mean daily, (b) pentad, and (c) 10-day precipitation averaged for 92 stations. Globally there has been no statistically significant overall trend in precipitation over the past century, although trends have varied widely by region and over time. Furthermore, mean annual precipitation decreases from north to south (Seasonal change of (a) mean daily, (b) pentad, and (c) 10-day precipitation averaged for 92 stations. Contours are every 20 m, but values from −10 to 10 m are not plotted.

Mean 10-day rainfall values are calculated from raw data for each station. Since the stationary Rossby wave was climatologically phase locked in seasonal evolution and the mean amplitude reached a maximum around the middle of July as shown in On the other hand, the anomalous high R2 at 500 hPa does not spread to the easternmost area of Mongolian in the break year as shown in Three stations without the break period around the Khenty Mountains (H in As shown in On the other hand, the anomalous high R2 at 500 hPa is predominant over western Mongolian in the break years in Seasonal and interannual variation of rainfall over Mongolia was analyzed using 9-yr twice-daily rainfall data and NCEP–NCAR reanalysis data. As a raindrop increases in size, its shape becomes more oblate, with its largest cross-section facing the oncoming airflow. Download citation file:Seasonal and interannual variation of rainfall over Mongolia was investigated using 10-day rainfall data from 92 stations during 1993–2001 and NCEP–NCAR reanalysis data from 1979 to 2001. Contours are every 2.5 m sThe break in 2000 was observed at the end of July, which is 10 days later than the climatological mean (As for the middle of July in 1997, the break was not only observed, but 10-day rainfall reached a maximum (These facts indicate that the break in the Mongolian rainy season is caused by the stationary Rossby wave trapped in the Asian jet, and the interannual variation of the break is also caused by variation of the stationary Rossby wave. The rainy season is the planting season in our country. In the break period, the stationary Rossby wave trapped in the Asian jet was predominant at 200 hPa, and a barotropic ridge associated with the Rossby wave developed over Mongolia.

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