Analysis of direct comparison of cloud top temperature and infrared split window signature against independant retrievals of cloud thermodynamic phase.

An accurate determination of cloud particle phase is required for retrieval of other cloud properties. The main purpose of this letter is to demonstra te that the cloud phase assumption made in previous cirrus clouds retrieval s using infrared split window signatures is not relevant. Coincident observ ations of the Earth surface from ERS-2 and ADEOS-1 satellites give us the o pportunity to compare clouds infrared signatures, as observed by ATSR-2 onb oard ERS-2, with cloud thermodynamic phase derived from POLDER onboard ADEO S-1. We find out, firstly, that large Brightness Temperature Differences (B TD), estimated between 11 and 12 mum, may occured for cold liquid water clo uds consisting of small supercooled droplets (i.e. altostratus). These BTDs have no longer been attributed to cirrus clouds as previous studies have b een. Secondly, the probability to observe ice or water clouds with respect to their cloud top temperature is quantified for our data set. A sharp tran sition between the ice and water phase is shown for cloud top temperatures ranging between 240 and 260 K. The probability for a cloud to be composed o f super-cooled liquid droplets is shown to be higher over land than over oc ean. This points out that ice activation susceptibility is more efficient i n maritime air mass than in continental one.