Diabatic processes modifying potential vorticity in a North Atlantic cyclone

By J. Chagnon, S. Gray, J. Methven. 2013

134 citations recorded by the source corpus.

How researchers see this paper

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

The North Atlantic Waveguide and Downstream Impact Experiment (2018, background): “In addition, a sharp peak in longwave radiative cooling near the tropopause, associated with a step change in water vapor, creates a reinforcement of the positive PV anomaly in upper-level troughs (Chagnon et al. 2013) and plays a key role in maintaining and strengthening TPVs (Cavallo and Hakim 201”
Clouds, circulation and climate sensitivity (2015, background): “…oscillations and mid-latitude jets 25,32,45,46 and inﬂuence the rate of development, the structure and the strength of smaller-scale disturbances such as tropical and extra-tropical cyclones, as well as the organization of convection and the occurrence of a range of mesoscale phenomena 1,41,47,48 .”
Blocking and its Response to Climate Change (2018, background): “decay of anomalies, but the vertical structure of long-wave cooling might actually act to enhance upper tropospheric anticyclonic anomalies [47].”