Responses of midlatitude blocks and wave amplitude to changes in the meridional temperature gradient in an idealized dry GCM
By Pedram Hassanzadeh, Z. Kuang, B. Farrell. 2014
140 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/c4d253ef0efd1000d75d18c5c6c1152b7f909ff6
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
- T. Woollings
- B. Hoskins
- Valerio Lucarini
- Michael Ghil
- Jiacan Yuan
- Robert E Kopp
- Elizabeth A. Barnes
- E. Tyrlis
In Global and Planetary Change
- T. Woollings
- Valerio Lucarini
- Michael Ghil
- B. Hoskins
- Jiacan Yuan
- R. Shwom
- Robert E Kopp
- Gernot Wagner
Citations in the corpus
- Tipping elements and climate–economic shocks: Pathways toward integrated assessment (2016, background): “However, some studies argue that the chance of mid-latitude cold extremes should decrease in response to future sea ice loss [Hassanzadeh et al., 2014; Screen et al., 2014].”
- The physics of climate variability and climate change (2019, background): “standard quasi-geostrophic ow theory,1 and lower jet speeds A favor blocking. But considerable evidence against this apparently straightforward argument has accumulated, too (Barnes and Screen, 2015; Hassanzadeh et al., 2014, and references therein). The existence of a nontrivial relation between in”
- Persistent Extratropical Regimes and Climate Extremes (2015, result): “[50] have led the field in this area with simple dynamical model experiments showing a reduction in wave amplitude as the meridional temperature gradient weakens, in contrast to the Francis and Vavrus hypothesis.”