Abstract
Observations are presented of a phenomenal upper tropospheric mesoscale temperature perturbation arising from the interaction between dissipating Tropical Cylone Kerry (1979) and a midlatitude trough in the westerlies which we describe as a black hole from its appearance on satellite imagery. We propose that this perturbation arose from dynamically forced subsidence along a confluence between the environmental flow and outflow from a major convective complex. The frequency of occurrence and subsequent adjustment of the atmosphere is described and discussed.-Authors
| Original language | English |
|---|---|
| Pages (from-to) | 1074-1082 |
| Number of pages | 9 |
| Journal | Monthly Weather Review |
| Volume | 112 |
| Issue number | 5 |
| DOIs | |
| State | Published - 1984 |