Humid continental climate
A humid continental climate (Köppen prefix D and a third letter of a or b) is a climatic region defined by Russian German climatologist Wladimir Köppen in 1900, which is typified by large seasonal temperature differences, with warm to hot (and often humid) summers and cold (sometimes severely cold) winters. Precipitation is usually well distributed through the year. The definition of this climate regarding temperature is as follows: the mean temperature of the coldest month must be below −3 °C (26.6 °F) and there must be at least four months whose mean temperatures are at or above 10 °C (50 °F). In addition, the location in question must not be semi-arid or arid.
Humid continental climates tend to be found above 30° N latitude to 60° N latitude, within the central and northeastern portions of North America, Europe, and Asia. They are much less commonly found in the Southern Hemisphere due to the larger ocean area at that latitude and the consequent greater maritime moderation. In the Northern Hemisphere some of the humid continental climates, typically in Scandinavia, Nova Scotia, and Newfoundland are heavily maritime-influenced, with relatively cool summers and winters being just below the freezing mark. More extreme humid continental climates found in southern Siberia and the American Midwest combine hotter summer maxima and colder winters than the marine-based variety. In some areas there are both strong subtropical and subarctic air mass influences depending on season, like the humid and hot summers and the frigid winters of Milwaukee, Wisconsin in the Upper Midwest of the United States.
Climatological averages are used to determine which locations are within a certain climate regime. The World Meteorological Organization has defined this average as through a 30 year period. The version from 1936 utilized a mean temperature of the coldest month of below −3 °C (26.6 °F) and there must be at least four months whose mean temperatures are at or above 10 °C (50 °F). These temperatures were not arbitrary. In Europe, the −3 °C (26.6 °F) average temperature isotherm (line of equal temperature) was near the southern extent of winter snowpack. The 10 °C (50.0 °F) average temperature was found to be the minimum temperature necessary for tree growth. Large temperature ranges are common within this climate zone.
In addition, the location in question must not be semi-arid or arid. Many climatologists in the U.S. prefer to use 0 °C (32 °F) as the standard because they feel it better reflects consistency in regional landscapes. This is from an update to the climate regime definition introduced by Trewartha & Horn in 1980. Despite the 1980 update, climate regimes are essentially the same within the Southern Hemisphere. The largest changes are seen in North America, Europe, and northern Asia.
Under Köppen, the following variants of this climate are possible. The climate regime uses a three letter code, beginning with the letter D. Otherwise,
- The second letter
- f : Does not meet either of the alternative specifications.
- s : A dry summer — the driest summer month has at most 30 millimetres (1.18 in) of rainfall and has at most 1⁄3 the precipitation of the wettest winter month.
- w : A dry winter — the driest winter month has at most one‑tenth of the precipitation found in the wettest summer month.
- The third letter
- a : Warmest month averages above 22 °C (71.6 °F)
- b : Does not meet the requirements for a, but there still are at least four months above 10 °C (50 °F).
Within North America, moisture within this climate regime is supplied by the Gulf of Mexico and adjacent western subtropical Atlantic. Precipitation is relatively well distributed year-round in many areas with this climate (f), while others may see a marked reduction in wintry precipitation, which increases the chances of a wintertime drought (w). Snowfall occurs in all areas with a humid continental climate and in many such places is more common than rain during the height of winter. In places with sufficient wintertime precipitation, the snow cover is often deep. Most summer rainfall occurs during thunderstorms, and in North America a very occasional tropical system. Though humidity levels are often high in locations with humid continental climates, the "humid" designation means that the climate is not dry enough to be classified as semi-arid or arid. The areas with a humid continental climate fall in the Dsa or Dsb categories are adjacent to Mediterranean climates where the elevation precludes such classification due to colder winters.
By definition, forests thrive within this climate. Biomes within this climate regime include temperate woodlands, temperate grasslands, temperate deciduous, temperature evergreen forests, and coniferous forests. Within wetter areas, spruce, pine, fir, and oak can be found. Fall foliage is noted during the autumn.
Hot/warm summer subtype
A hot (or warm) version of a continental climate features an average temperature of at least 22 °C (71.6 °F) in its warmest month. Since these regimes are limited to the Northern Hemisphere, the warmest month is usually July or August. In this region, July afternoon temperatures average up to 32 °C (90 °F), while the January mean temperature can be far below −3.0 °C (26.6 °F). Frost free periods normally last 5-6 months within this climate regime.
Within North America, it includes small areas of southeast Canada and portions of the eastern United States from the Atlantic to the 100th meridian, and in the general range of between 39 °N to 44 °N latitude (with a larger north-south spread in the western portion due to the lack of maritime influences); precipitation increases further eastward in this zone and is less seasonally uniform in the west. The western states of the central United States (namely Montana, Wyoming, parts of southern Idaho, parts of Colorado, parts of Utah,western Nebraska, and parts of western North and South Dakota) have thermal regimes which fit the Dfa climate type, but are quite dry, and are generally grouped with the steppe (BSk) climates.
|Climate chart (explanation)|
In the Eastern Hemisphere, this climate regime is found within interior Eurasia, east-central Asia, and parts of India. Within Europe, the Dfa climate type is present near the Black Sea in southern Ukraine, the Southern Federal District of Russia, southern Moldova, Serbia, parts of southern Romania, and Bulgaria, but tends to be drier and can be even semi-arid in these places. In East Asia, this climate exhibits a monsoonal tendency with much higher precipitation in summer than in winter, and due the effects of the strong Siberian High much colder winter temperatures than similar latitudes around the world, however with lower snowfall, the exception being western Japan with its heavy snowfall. 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 relatively 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. Much of central Asia, northwestern China, and southern Mongolia have a thermal regime similar to that of the Dfa climate type, but these regions receive so little precipitation that they are more often classified as steppes (BSk) or deserts (BWk).
Mild/cool summer subtype
|Climate chart (explanation)|
Areas featuring this subtype of the continental climate have an average temperature in the warmest month below 22 °C. Summer high temperatures in this zone typically average between 21–28 °C (70–82 °F) during the daytime and the average temperatures in the coldest month are generally far below the −3 °C (27 °F) isotherm. Frost-free periods typically last 3–5 months. Heat spells lasting over a week are rare. Winters are brisk and cold.
The cool summer version of the humid continental climate covers a much larger area than the hot subtype. In North America, the climate zone covers from about 44°N to 50°N latitude mostly east of the 100th meridian. However, it can be found as far north as 54°N, and further west in the Canadian Prairie Provinces and below 40°N in the high Appalachians. In Europe this subtype reaches its most northerly latitude at nearly 61° N.
In the Western Hemisphere, high-altitude locations as South Lake Tahoe, California and Aspen, Colorado in the western United States exhibit local Dfb climates. The south-central and southwestern Prairie Provinces also fits the Dfb criteria from a thermal profile, but because of semi-arid precipitation portions of it are grouped into the BSk category.
|Climate chart (explanation)|
In Europe, it is found in Poland, Russia, the Nordic countries of Sweden and Finland, Norway, Estonia, Latvia, Lithuania, Slovakia, and eastern Hungary. It has little warming or precipitation effects from the northern Atlantic. The cool summer subtype is marked by mild summers, long cold winters and less precipitation than the hot summer subtype; however, short periods of extreme heat are not uncommon. Northern Japan has a similar climate.
In the Southern Hemisphere it exists in well-defined areas only in the Southern Alps of New Zealand, the Snowy Mountains of Australia, Kiandra, New South Wales, and perhaps[vague] as isolated microclimates of the southern Andes of Chile and Argentina.
Use in climate modeling
Since climate regimes tend to be dominated by vegetation of one region with relatively homogenous ecology, those that project climate change remap their results in the form of climate regimes as an alternative way to explain expected changes.
- Michal Belda, Eva Holtanová, Tomáš Halenka, and Jaroslava Kalvová (2014-02-04). "Climate classification revisited: from Köppen to Trewartha" (PDF). Climate Research 59: 1–14.
- Béla Berényi. Cultivated Plants, Primarily As Food Sources -- Vol II -- Fruit in Northern Latitudes (PDF). Encyclopedia of Life Support Systems. p. 1. Retrieved 2015-02-23.
- "Halifax, Nova Scotia Temperature Averages". Weatherbase. Retrieved 7 February 2015.
- "Milwaukee, Wisconsin Temperature Averages". Weatherbase. Retrieved 7 February 2015.
- Antonio Ribeiro da Cunha and Edgar Ricardo Schöffel (November 2011). "20". Measurements to Agricultural and Environmental Applications (PDF). InTech. pp. 392–396. ISBN 978-953-307-512-9. Retrieved 2015-02-22.
- C. Donald Ahrens and Robert Henson (2015-01-01). Meteorology Today (11 ed.). Cengage Learning. pp. 491–492. ISBN 1305480627. Retrieved 2015-02-23.
- Steven Ackerman and John Knox (2006-03-08). Meteorology: Understanding the Atmosphere. Cengage Learning. p. 419. ISBN 1305147308. Retrieved 2015-02-23.
- "Updated world map of China and Japan, and Syria, the Köppen-Geiger climate classification" (PDF). University of Melbourne. Retrieved February 22, 2011.
- Andy D. Ward, Stanley W. Trimble (2003-12-18). Environmental Hydrology, Second Edition. CRC Press. pp. 31–34. ISBN 1566706165. Retrieved 2015-02-23.
- Vijendra K. Boken, Arthur P. Cracknell, and Ronald L. Heathcote (2005-03-24). Monitoring and Predicting Agricultural Drought : A Global Study: A Global Study. Oxford University Press. p. 349. ISBN 0198036787. Retrieved 2015-02-18.
- Timothy Champion, Clive Gamble, Stephen Shennan, and Alisdair Whittle (2009-08-15). "Prehistoric Europe". Left Coast Press. p. 14. ISBN 1598744631. Retrieved 2015-02-23.
- Gordon B. Bonan (2008-09-18). "6". Ecological Climatology: Concepts and Applications. Cambridge University Press. ISBN 1107268869. Retrieved 2015-02-23.
- National Climatic Data Center. "Illinois Normals" (PDF). National Oceanic and Atmospheric Administration. Retrieved 2015-02-23.
- Joseph Hobbs (2012-07-13). Fundamentals of World Regional Geography. Cengage Learning. p. 76. ISBN 1285402219. Retrieved 2015-02-23.
- Michael Kramme, Ph.D. (2012-01-03). Exploring Europe, Grades 5 - 8. Carson-Dellosa Publishing. p. 12. ISBN 1580376703. Retrieved 2015-02-23.
- Peel, M. C. and Finlayson, B. L. and McMahon, T. A. (2007). "Updated world map of the Köppen–Geiger climate classification". Hydrol. Earth Syst. Sci. 11: 1633–1644. ISSN 1027-5606. (direkt: Final Revised Paper; PDF; 1,7 MB)