Mohawk–Hudson convergence
id:
mohawk-hudson-convergence-235-7147119
title:
Mohawk–Hudson convergence
text:
Mohawk–Hudson convergence (MHC) is a mesoscale meteorology phenomenon occurring over the Capital District region of upstate New York, United States. The small convergence zone forms within specific weather conditions sometimes found in the wake of extratropical cyclones shifting east of the area. Given air pressure decreasing with both longitude and latitude, as well as weak synoptic low-level flow, winds are channeled east along the Mohawk Valley and south through the Hudson Valley, converging
brand slug:
wiki
category slug:
encyclopedia
description:
original url:
https://en.wikipedia.org/wiki/Mohawk%E2%80%93Hudson_convergence
date created:
date modified:
2023-08-01T19:24:37Z
main entity:
{"identifier":"Q17081643","url":"https://www.wikidata.org/entity/Q17081643"}
image:
{"content_url":"https://upload.wikimedia.org/wikipedia/commons/f/f5/Mohawk_and_Hudson_Valleys.jpg","width":5184,"height":4088}
fields total:
13
integrity:
14