Amir Mohsen
متخصص بخش هواشناسی
آپدیت جدید نقشه ها و ارتفاع ژئوپتانسیل:
Temperature Advection 700 hPa Temperature Advection indicates the movement of warmer/colder air into regions with colder/warmer on a horizontal level. The regions with cold air advection are marked by blue solid lines. Warm air advection in red solid lines.
CAPE
CAPE which stands for Convective Available Potential Engergy (CAPE) is defined as the vertically integrated positive buoyancy of a rising parcel. Unlike with the Lifted Index where the difference between the lifted air parcel and the actual observed temperature was calculated at only 500 hPa., with CAPE the differences is calculated and integrated over all levels.
CAPE isolines are shown for 100,200 and 400 J Kg[SUP]-1[/SUP] in yellowish orange, for 800 J Kg[SUP]-1[/SUP] in tangerine, for 1200 J Kg[SUP]-1[/SUP] in pink, for 1600 J Kg[SUP]-1[/SUP] in rose, for 2000 J Kg[SUP]-1[/SUP] in lavender, for 2500 J Kg[SUP]-1[/SUP] in magenta, for 3000 in violet and for 4000 J Kg[SUP]-1[/SUP] in purple colours.
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Temperature Advection 700 hPa Temperature Advection indicates the movement of warmer/colder air into regions with colder/warmer on a horizontal level. The regions with cold air advection are marked by blue solid lines. Warm air advection in red solid lines.
CAPE
CAPE which stands for Convective Available Potential Engergy (CAPE) is defined as the vertically integrated positive buoyancy of a rising parcel. Unlike with the Lifted Index where the difference between the lifted air parcel and the actual observed temperature was calculated at only 500 hPa., with CAPE the differences is calculated and integrated over all levels.
CAPE isolines are shown for 100,200 and 400 J Kg[SUP]-1[/SUP] in yellowish orange, for 800 J Kg[SUP]-1[/SUP] in tangerine, for 1200 J Kg[SUP]-1[/SUP] in pink, for 1600 J Kg[SUP]-1[/SUP] in rose, for 2000 J Kg[SUP]-1[/SUP] in lavender, for 2500 J Kg[SUP]-1[/SUP] in magenta, for 3000 in violet and for 4000 J Kg[SUP]-1[/SUP] in purple colours.
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