Impact of monsoon circulations on the upper troposphere and lower stratosphere

By Andrew Gettelman, Douglas E. Kinnison, T. Dunkerton, G. Brasseur. 2004

231 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/4c117c0e696e0bffdb0e33f220eafb5d7c63ab7e

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

1. William J. Randel
2. Andrew Gettelman
3. S. Fueglistaler
4. M. Hegglin
5. Q. Fu
6. P. Konopka
7. L. Pan
8. T. Dunkerton

In Global and Planetary Change

1. William J. Randel
2. Andrew Gettelman
3. Q. Fu
4. M. Hegglin
5. P. Konopka
6. L. Pan
7. S. Fueglistaler
8. Andrew E. Dessler

Citations in the corpus

• Observations of deep convective influence on stratospheric water vapor and its isotopic composition (2007, background): “Another possibility is that the convective outflow at q = 380 K in the Asian monsoon region is transported equatorward and joins into the general circulation of the stratosphere [Gettelman et al., 2004; Fu et al., 2006].”
• Tropical tropopause layer (2009, background): “However, the altitude of the clear-sky LZRH shows little variation in the tropics [Gettelman et al., 2004a].”
• Deep convective influence on the Asian summer monsoon anticyclone and associated tracer variability observed with Atmospheric Infrared Sounder (AIRS) (2006, background): “The monsoon circulation also probably plays an important role in stratosphere-troposphere exchange (STE) during summer [Dethof et al., 1999; Bannister et al., 2004; Gettelman et al., 2004a].”
• CALIPSO detection of an Asian tropopause aerosol layer (2011, unknown): “[Gettelman et al., 2004; Randel et al., 2010].”
• Impact of the vertical velocity scheme on modeling transport in the tropical tropopause layer (2010, background): “Above the level of zero radiative heating (LZRH), at about 360 K, the Brewer-Dobson circulation causes further ascent to the stratospheric overworld [Holton et al., 1995], balanced by positive radiative heating [Gettelman et al., 2004a].”
• THE EXTRATROPICAL UPPER TROPOSPHERE AND LOWER STRATOSPHERE (2011, background): “The anticyclonic circulation is also linked to persistent quasi ‐ horizontal transport between the tropics and extratropics upstream and downstream of the anticyclone [ Gettelman et al. , 2004; Konopka et al. , 2009].”
• Horizontal water vapor transport in the lower stratosphere from subtropics to high latitudes during boreal summer (2013, background): “Recent studies have shown evidence for the Asian monsoon to act as an efficient transport pathway into the lower stratosphere [Gettelman et al., 2004; Randel et al., 2010].”
• Satellite-Based Atmospheric Infrared Sounder Development and Applications (2017, methodology): “UTWV products from hyperspectral sounders have also been applied to the study of seasonal variance in monsoon regions (Gettelman et al. 2004), model assessment (Takahashi et al.”