Humid continental climate
id:
humid-continental-climate-184-4580244
title:
Humid continental climate
text:
A humid continental climate is a climatic region defined by Russo-German climatologist Wladimir Köppen in 1900, typified by four distinct seasons and large seasonal temperature differences, with warm to hot summers, and cold and snowy winters. Precipitation is usually distributed throughout the year, but often these regions do have dry seasons. The definition of this climate in terms of temperature is as follows: the mean temperature of the coldest month must be below 0 °C (32.0 °F) or −3 °C (26
brand slug:
wiki
category slug:
encyclopedia
description:
Category in the Köppen climate classification system
original url:
https://en.wikipedia.org/wiki/Humid_continental_climate
date created:
2004-11-30T07:15:08Z
date modified:
2024-09-07T17:23:27Z
main entity:
{"identifier":"Q10856115","url":"https://www.wikidata.org/entity/Q10856115"}
image:
{"content_url":"https://upload.wikimedia.org/wikipedia/commons/4/4e/Koppen-Geiger_Map_v2_D_1991%E2%80%932020.svg","width":1401,"height":928}
fields total:
13
integrity:
16