U. Lohmann et al., THE ROLE OF WATER-VAPOR AND CONVECTION DURING THE CENTRAL EQUATORIAL PACIFIC EXPERIMENT FROM OBSERVATIONS AND MODEL SIMULATIONS, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 100(D12), 1995, pp. 26229-26245
Field measurements from the Central Equatorial Pacific Experiment (CEP
EX) conducted from March 7 to April 5, 1993, are used to study the lin
k between water vapor, convection, and sea surface temperature (SST) i
n a region of particular importance to global climate. The data are co
mpared with results from a general circulation model (GCM). Three high
-resolution simulations were carried out with slightly different initi
al conditions using European Centre for Medium Range Weather Forecasts
(ECMWF) analyses from March 1, 1993, and forced with the observed SST
as lower boundary condition. Radiosondes released between the equator
and 5 degrees S show a dry region east of the dateline collocated wit
h a clear sky region observed from the Japanese Geostationary Meteorol
ogical Satellite (GMS) in the first 2 weeks of CEPEX, which both vanis
h in the second 2 weeks. The model is able to reproduce this change in
convective activity, Moreover, a comparison of the anomalies of the r
elative humidity profiles grouped according to SST and infrared bright
ness temperature (IRBT) indicates that the GCM correctly simulates the
observed behavior, The atmosphere is relatively moist when the SST is
warm and low IRBTs occur at the same time, that is, when convection t
akes place, and dryer than on average for the opposite case. In genera
l, however, the model is too dry in the midtroposphere and too wet in
the upper troposphere. Very good agreement is found between the simula
ted and observed ice water content, in particular with respect to its
increase with in-cloud temperature.