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Summer is the period of maximum rain, which is less abundant than in the west; in both the north and southeast of the East European Plain, precipitation reaches only between 10 and 20 inches (250 and 500 mm) annually.
There is a building in Bristol which we installed using this idea with partitions to capture maximum rain water which feeds into a glass valley and is then filtered back into the house.
An analysis of their study indicates the increasing trend of daily maximum rain in the Amazon basin.
On the other hand, the southern parts of the country are receiving maximum rain during the months of March to May and a similar trend has recorded.
In addition, the maximum rain attenuation experienced in Ka systems has a difference about 5 dB (of peak reduction) between the attenuation affecting the best and worst locations[5].
A very rough evaluation of the maximum rain intensity may be obtained by assuming that the raindrops fall with a velocity of 9 m/s (characteristic value for the velocity of large raindrops; see Gunn and Kinzer 1949) from a typical condensation level altitude of 3000 m; it takes 666 s for the rain drops to reach the ground.
Similar(52)
Average annual rainfall is 489 mm, with March recording the maximum (with rain snow and sleet for 11 days) of 664 mm and July is the driest month with rainfall of 0.1 inches.
As indicated in the observation (NNRP), the southwestern and central highlands of Ethiopia received maximum summer rain; whereas, the eastern, western and southeastern periphery of the country has received very little summer rain.
Interestingly, we found that for 9 out of the 11 paired hillslopes, 40 70% of the temporal variation in the scaling factors can be explained by the antecedent wetness condition and the maximum hourly rain accumulation.
The HI seems to predict several tens of minutes of the maximum observed rain, located between 11 00 and 12 00 UTC in hourly histograms, and ARPAL, the regional agency for environmental protection, describes the event with the radar image of 11 35 UTC (ARPAL 2012).
Second, the remaining (non-annual maximum) rainfall is rescaled such that the mass balance of the generated rain before and after scaling is maintained.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com