Seasonal variation and environmental properties of southward propagating mesoscale convective systems over the Bay of Bengal

T Miyakawa, T Satomura - SOLA, 2006 - jstage.jst.go.jp
T Miyakawa, T Satomura
SOLA, 2006jstage.jst.go.jp
The numbers of fast moving MCSs were as follows: April 11/56 (20%); May 46/103 (45%);
June 50/173 (29%); July 33/160 (21%); August 27/125 (22%); September 8/61 (13%);
October 8/67 (12%); total 183/745 (25%). The fractions represent (number of southward
propagating MCSs)/(total number of MCSs), and the numbers inside the parentheses are the
percentages of the southward propagating MCSs. We concluded that fast southward
propagation of MCSs tends to occur when a trough exists over the Bay at the height of 600 …
The numbers of fast moving MCSs were as follows: April 11/56 (20%); May 46/103 (45%); June 50/173 (29%); July 33/160 (21%); August 27/125 (22%); September 8/61 (13%); October 8/67 (12%); total 183/745 (25%). The fractions represent (number of southward propagating MCSs)/(total number of MCSs), and the numbers inside the parentheses are the percentages of the southward propagating MCSs. We concluded that fast southward propagation of MCSs tends to occur when a trough exists over the Bay at the height of 600 hPa, and the wind shear between the surface and the 600 hPa height has a southward component. We also found that propagation towards other directions is related with eddy disturbances over the Bay.
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