Dynamical Mechanism for the Increase in Tropical Upwelling in the Lowermost Tropical Stratosphere during Warm ENSO Events

By N. Calvo, R. Garcia, William J. Randel, D. Marsh. 2010

168 citations recorded by the source corpus.

Subfields: Astronomy and Astrophysics, Atmospheric Science

View Paper: https://www.semanticscholar.org/paper/25f3c5ed863fd562b3e7f0656088df3d084096c3

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Astronomy and Astrophysics

1. D. Marsh
2. Douglas E. Kinnison
3. J. Richter
4. R. Garcia
5. Han-Li Liu
6. S. Solomon
7. L. Polvani
8. William J. Randel

In Atmospheric Science

1. Andrew Gettelman
2. R. Garcia
3. C. Garfinkel
4. Douglas E. Kinnison
5. A. Butler
6. William J. Randel
7. D. Marsh
8. J. Richter

Citations in the corpus

• The Teleconnection of El Niño Southern Oscillation to the Stratosphere (2019, background): “During an El Niño event, anomalous upward propagation and dissipation of planetary waves at middle and high latitudes and gravity waves in the subtropics (Calvo et al., 2010; Garfinkel & Hartmann, 2008) leads to a strengthening of the Brewer-Dobson circulation, resulting in a cooler tropical lower s”
• The Whole Atmosphere Community Climate Model Version 6 (WACCM6) (2019, background): “Prior studies with WACCM include trends resulting from increasing greenhouse gases (e.g., Garcia et al., 2007), the climatology of the tropical tropopause layer (Gettelman & Birner, 2007), the response of the atmosphere to the solar cycle and the flux of energetic particles (e.g., Jackman et al., 20”