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To achieve this aim, we use a new Convective/Stratiform Rain Area Delineation Technique (CS-RADT).
The radiance ratio of Ch1Ch2 also shows a good correspondence to the PR and TMI rain area.
Sensitive experiments demonstrate that the flow dependent background error covariance and the ensemble mean background field are both the key factors for adding effective mesoscale information to the heavy rain area, and they are both essential for improving the heavy rain forecasts.
Firstly, the trend of the acid rain in East Asia due to the rapid increase of Chinese pollutants emission was investigated, and a remarkably rapid increase of acid rain area was predicted in the period from 1985 to 1995, the monthly mean pH values showing the decrease of 0.3 0.8 in the area from the center to northeast in China, and 0.1 0.2 even in Japan and Korea.
Open image in new window Fig. 6 Delineated rain area for the scene from Mars 09, 2011 (12 30 UTC). a BT10.8 image, b rain area delineated by Radar and MLP c rain area detected by Radar and ECST.
Open image in new window Fig. 3 MLP for rain area delineation.
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The degree of severity of each storm event for the city is shown to depend also on the extent of heavy rain areas and therefore on the spatial structure of rainfall intensities.
Correlation scales were analyzed for rain-free areas, weak rain areas, and heavy rain areas by dividing the rain rates (R [mm/h]) into three intensity levels, i.e., R < 0.1, 0.1 ≤ R < 10, R ≥ 10.
In this paper, a new method to delineate rain areas in northern Algeria is presented.
Figure 5b and c shows the rain areas delineated by SI and MLP, respectively.
It was found that the e-folding scales of correlations were 30.8, 7.5, and 4.8 km for the rain-free, weak rain, and heavy rain areas, respectively.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com