Convective cell detection

22 June 2007, 1830 UTC - 23 June2007, 0400 UTC

22 June 2007, 1830 UTC
Convective cells are detected based upon their temperature, shape and the difference between the cloud top temperature of the cell and its surroundings. The weakness of this method is the fact that the IR signal gives only the temperature of the top, regardless of the type of the cloud beneath (meaning that the cirrus clouds can also be considered as convective). This effect is eliminated by some extent by considering the shape (only the round and oval shaped structures are analyzed) and the difference from the surrounding pixels (the cloud has to "stick out" from the surrounding). Regarding the shape and size of the cells, problems sometimes occur when the cells are very big and flat. If there is a large area with low temperature the cell will not be detected. This is the reason why the signs for the cells suddenly  "disappear" and then "reappear" in some of the next time steps, although the cell itself is visible in every image.


At the beginning of the convection over Croatia convective cells are detected over the north Adriatic. The sign for the cell disapears after 20:00 UTC when the cell has grown rather large. Many cells are detected between 22:00 and 03:00 UTC when the majority of convection happened.