Diurnal cycle of convection, clouds, and water vapor in the tropical upper troposphere: Satellites versus a general circulation model
By Baijun Tian, Brian J. Soden, Xiangqian Wu. 2004
201 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/9f15796c44bbe80830ead90c73ef411a31fb273a
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Atmospheric Science
- M. Webb
- Sandrine Bony
- J. Dufresne
- Brian J. Soden
- M. Zelinka
- Stephen A. Klein
- Chris Bretherton
- Richard P. Allan
In Global and Planetary Change
- M. Webb
- Sandrine Bony
- J. Dufresne
- M. Zelinka
- Brian J. Soden
- Stephen A. Klein
- Chris Bretherton
- D. Hartmann
Citations in the corpus
- How Well Do We Understand and Evaluate Climate Change Feedback Processes (2006, background): “…ability of climate models to reproduce cloud variations observed at the diurnal (Yang and Slingo 2001; Dai and Trenberth 2004; Slingo et al. 2004; Tian et al. 2004), seasonal (Tsushima and Manabe 2001; Zhang et al. 2005), interannual (Potter and Cess 2004; Ringer and Allan 2004) and decadal…”
- Diurnal Variation in Precipitation over India during the Summer Monsoon Season: Observed and Model Predicted (2007, background): “In the Tropics most of the rainfall is from the tall clouds (Cu or Cb) formed by convection within a deep layer of the atmosphere.”
- A simple method to relate microwave radiances to upper tropospheric humidity (2005, methodology): “[7] Quite a number of studies have used the BT transformation method to transform infrared radiances into UTH [Escoffier et al., 2001; Tian et al., 2004; Bates and Jackson, 2001; Soden et al., 2004], including a recent study on humidity supersaturation with respect to ice as seen by the…”