Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/95337/1/jgrd16515.pd
The coupling between sea surface temperature (SST) anomalies and rainfall is an important driver of ...
Published under Creative Commons Licence 3.0. Original article can be found at : http://www.atmosphe...
Water vapor distributions obtained from the fourth generation ECHAM general circulation model are co...
Measuring and simulating moist processes in the tropical upper troposphere are difficult tasks. Humi...
The factors that control the influence of deep convective detrainment on water vapor in the tropical...
The factors that control the influence of deep convective detrainment on water vapor in the tropical...
The factors that control the influence of deep convective detrainment on water vapor in the tropical...
The tropical deep overshooting convection is known to be most intense above continental areas such a...
The vertical temperature structure in the tropics is primarily set by convection and therefore follo...
International audienceDiurnal variations of upper tropospheric humidity (UTH) as well as middle trop...
Measuring and simulating moist processes in the tropical upper troposphere are difficult tasks. Humi...
Controversy remains over a discrepancy between modeled and observed tropical upper tropospheric temp...
Fast convective transport in the tropics can efficiently redistribute water vapour and pollutants up...
Ten years (1994–2004) of measurements of tropical upper-tropospheric water vapor (UTWV) by the Measu...
We present the time mean heat budgets of the tropical upper troposphere (UT) and lower stratosphere ...
The coupling between sea surface temperature (SST) anomalies and rainfall is an important driver of ...
Published under Creative Commons Licence 3.0. Original article can be found at : http://www.atmosphe...
Water vapor distributions obtained from the fourth generation ECHAM general circulation model are co...
Measuring and simulating moist processes in the tropical upper troposphere are difficult tasks. Humi...
The factors that control the influence of deep convective detrainment on water vapor in the tropical...
The factors that control the influence of deep convective detrainment on water vapor in the tropical...
The factors that control the influence of deep convective detrainment on water vapor in the tropical...
The tropical deep overshooting convection is known to be most intense above continental areas such a...
The vertical temperature structure in the tropics is primarily set by convection and therefore follo...
International audienceDiurnal variations of upper tropospheric humidity (UTH) as well as middle trop...
Measuring and simulating moist processes in the tropical upper troposphere are difficult tasks. Humi...
Controversy remains over a discrepancy between modeled and observed tropical upper tropospheric temp...
Fast convective transport in the tropics can efficiently redistribute water vapour and pollutants up...
Ten years (1994–2004) of measurements of tropical upper-tropospheric water vapor (UTWV) by the Measu...
We present the time mean heat budgets of the tropical upper troposphere (UT) and lower stratosphere ...
The coupling between sea surface temperature (SST) anomalies and rainfall is an important driver of ...
Published under Creative Commons Licence 3.0. Original article can be found at : http://www.atmosphe...
Water vapor distributions obtained from the fourth generation ECHAM general circulation model are co...
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