Humid continental climate

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The humid continental climate is a climate found over large areas of land masses in the temperate regions of the mid-latitudes where there is a zone of conflict between polar and tropical air masses. The humid continental climate is marked by variable weather patterns and a large seasonal temperature variance. The seasonal temperature variance can be as great as 30-39° Celsius (55-70° Fahrenheit). The temperature difference between the warmest and coldest months increases as one moves further inland and away from the moderating influence of the ocean. Winter high temperatures are usually between 10 F and 45 F with lows between -10 F and 25 F. Summer high temperatures are usually between 70 F and 90 F with lows between 45 F and 65 F. Spring begins between Early March in southern parts of this zone to Mid April in Southern Canada.

[edit] Dfa: Warm summer subtype

Humid Continental Climate in the United States

The warm summer (Köppen: Dfa) subtype of the humid continental climate, marked by hot (the warmest month has an average temperature in excess of 22°C (71.6°F), rainy summers and snowy winters. Within North America it includes much of the eastern and midwestern portions of the United States and extreme southern Canada from the Atlantic to the 100th meridian west and from about 40°N to 44°N latitude; this area includes the following regions:

Most of New York state (except for the northern part and some highland areas in the southwest)
Northern New Jersey
Most of Pennsylvania (except for its southeastern region and some highland areas)
Extreme western Maryland (due to higher elevations)
Extreme western and southwestern Virginia (due to higher elevations)
Parts of Kentucky
Northern Arkansas
Western North Carolina (due to higher elevations)
Most of West Virginia (except high elevations)
Most of Ohio
Most of Indiana
Most of Illinois
Most of Missouri
Iowa
Eastern Nebraska
Eastern Kansas
Southern Minnesota
Southern Wisconsin
Southern Michigan
Southern Ontario (south of and including Toronto)
Connecticut
Rhode Island
Massachusetts (except for some mountainous locations, but see Cape Cod)
southern Vermont
southern New Hampshire

Some of the major cities in this zone:

The 0°C (32°F) isotherm (freeze line) or the -3°C (26.6°F) isotherms (persistent snow line) are the possible lines dividing the humid continental and the humid subtropical climates, in between which are the following places (which are often included in the humid continental zone)^{[citation needed]}:

Although the largest portion of territory on Earth covered by the Dfa climate type is present in North America, it also exists near the Black Sea in southern Ukraine, the Southern Federal District of Russia, Moldova and much of Romania within Europe, but tends to be drier. Tohoku in Japan between Tokyo and Hokkaidō also has a climate with Köppen classification Dfa, but is wetter even than that part of North America with this climate type. A variant which has dry winters and hence much lower snowfall with monsoonal type summer rainfall is to be found in north-eastern China including coastal regions of the Yellow Sea and over much of the Korean Peninsula; it has the Köppen classification Dwa.

Cities outside North America with this climate include:

[edit] Dfb: Cool summer subtype

The cool summer subtype (Köppen: Dfb) lies north of the warm summer subtype; in North America, from about 44°N to 50°N in the east but places of adequate precipitation as far north as 54°N in the Canadian Prairie Provinces and below 40°N in the high Appalachians, separated by the 22°C isotherm for the warmest month from the Dfa climates (which passes near Minneapolis, Minnesota and Grand Rapids, Michigan).Summer temperatures in this zone are usually between 70 F and 85 F during the daytime.

It includes the following places:

Central and Northern New England
Northern New York
Northern Michigan
Northern and central Wisconsin
Northern and central Minnesota
Eastern parts of The Dakotas
Highest elevations of the central Appalachians

In Canada, it includes these areas:

Most of Atlantic Canada
Southern Quebec
Most of Ontario except south of Toronto and far northern regions
Southern Manitoba
Central and southeastern Saskatchewan
Central (latitudinal) Alberta

Some of the major cities in this zone:

It is also found in central Scandinavia. East central Europe is a cool summer subtype with less severe winters, similar to the winters of the warm summer subtype - the winters here are modified by the oceanic climate influence of western Europe.

The cool summer subtype is marked by mild summers, long cold winters and less precipitation than the warm summer subtype, however, short periods of extreme heat are not uncommon. In this region, summers shorten and are cooler, and winters become longer and colder toward the north parts of this zone. Northern Japan has a similar climate.

Locations with such climates outside North America include:

A dry-winter variant (Köppen: Dwb) is to be found in northeastern China, northern Korea and the Southeastern region of Russian Far East, as at Vladivostok and Chongjin, North Korea, and Harbin, China.

[edit] Subarctic climate

Near 50°N in North America (except north of 55°N in Alberta and British Columbia) and eastern Asia (60°N or further north in Europe), the climate grades into a subarctic climate (Köppen: Dfc, Dwc), poleward of which the summers (seasons with temperatures above 10°C) are shorter than four months.

Climate types under the Köppen climate classification
Class A: Tropical (Af) - Monsoon (Am) - Savanna (Aw, As)
Class B: Arid (BWh, BWk) - Semi-arid (BSh, BSk)
Class C: Humid subtropical (Cfa, Cwa) - Oceanic (Cfb, Cwb, Cfc) - Mediterranean (Csa, Csb)
Class D: Humid continental (Dfa, Dwa, Dfb, Dwb) - Subarctic (Dfc, Dwc, Dfd) - High-altitude Mediterranean (Dsa, Dsb, Dsc)
Class E: Polar (ET, EF) - Alpine (ETH)

Retrieved from "http://en.wikipedia.org../../../h/u/m/Humid_continental_climate.html"

Humid continental climate

From Wikipedia, the free encyclopedia

[edit] Dfa: Warm summer subtype

[edit] Dfb: Cool summer subtype

[edit] Subarctic climate

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