Humid continental climate

, Japan, has a humid continental climate (Köppen Dfa). Using the Köppen climate classification, a climate is classified as humid continental when the temperature of the coldest month is below or and there must be at least four months whose mean temperatures are at or above . Wide temperature ranges are common within this climate zone. Second letter in the classification symbol defines seasonal rainfall as follows: • s: A dry summer—the driest month in the high-sun half of the year (April to September in the Northern Hemisphere, October to March in the Southern Hemisphere) has less than / of rainfall and has exactly or less than the precipitation of the wettest month in the low-sun half of the year (October to March in the Northern Hemisphere, April to September in the Southern Hemisphere). • w: A dry winter—the driest month in the low-sun half of the year has exactly or less than one‑tenth of the precipitation found in the wettest month in the summer half of the year. • f: No dry season—does not meet either of the alternative specifications above; precipitation and humidity are often high year-round. while the third letter denotes the extent of summer heat: Precipitation is relatively well distributed year-round in many areas with this climate (f), while others may see a marked reduction in wintry precipitation, 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, Within wetter areas, maple, spruce, pine, fir, and oak can be found. Fall foliage is noted during the autumn of deciduous forests. Neighboring climates In the poleward direction, these climates transition into subarctic climates featuring short summers (and usually very cold winters) allowing only conifer trees. Moving equatorword, the hot-summer continental climates grade into humid subtropical climates (chiefly in North America and Asia) while the warm-summer continental climates grade into oceanic climates (chiefly in Europe), both of which have milder winters where average temperatures stay above 0 °C (or -3 °C). Some continental climates with lower precipitation (chiefly in Central Asia and the Western United States) grade into semi-arid climates with similar temperatures but low precipitation. == Hot summer subtype ==

A hot summer 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 restricted to the Northern Hemisphere, the warmest month is usually July or August. High temperatures during the warmest month tend to be in the high 20s to low 30s °C (80s °F), while average January afternoon temperatures are near or well below freezing. Frost-free periods typically last 4 to 7 months in this climate regime. 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 to 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. Tōhoku on the western coast of Japan 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 northern China including Manchuria and parts of North China, far East of Russia, and over much of the Korean Peninsula; it has the Köppen classification Dwa. Much of central Asia, northwestern China, and southern Mongolia has 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). Dsa climates are rare; they are generally restricted to elevated areas adjacent to mid-latitude Mediterranean climate regions with a Csa climate well inland to ensure hot summers and cold winters. They are generally found in the highly elevated areas of south-eastern Turkey (Hakkâri), north-western Iran, northern Iraq, parts of Central Asia, parts of the High Atlas mountain range in central Morocco and parts of the Intermountain West in the United States. This climate zone does not exist at all in the Southern Hemisphere, where the continents either do not penetrate low enough in latitude or taper too much to have any place that gets the combination of snowy winters and hot summers. Marine influences are very strong around 40°S and such preclude Dfa, Dwa, and Dsa climates from existing in the southern hemisphere. {{climate chart {{climate chart {{climate chart {{climate chart == Warm summer subtype ==

Also known as hemiboreal climate, areas featuring this subtype of the continental climate have an average temperature in the warmest month below . Summer high temperatures in this zone typically average between during the daytime and the average temperatures in the coldest month are generally well or far below the (or ) isotherm. Frost-free periods typically last 3–5 months. Heat spells lasting over a week are rare. and below 40°N in the high Appalachians. In Europe, this subtype reaches its most northerly latitude in Bodø at the 67°N. High-altitude locations such as Flagstaff, Arizona, Aspen, Colorado and Los Alamos, New Mexico 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. In Europe, it is found in much of Central Europe: Germany (in the east and southeast part of the country), Austria (generally below ), Poland, Czech Republic, Slovakia, Hungary (generally above ), Croatia (mostly Slavonia region), in much of Eastern Europe: Ukraine (the whole country except the Black Sea coast), Belarus, Russia (mostly central part of European Russia), south and central parts of the Nordic countries not bathed by the Atlantic Ocean or North Sea: Sweden (historical regions of Svealand and Götaland), Finland (south end, including the three largest cities), It has little warming or precipitation effects from the northern Atlantic. In Asia, this climate type is found in northern Kazakhstan, southern Siberia, parts of Mongolia, northern China, and highland elevations in the Koreas. Like its hot-summer counterpart, these climates are typically dry in the winter and bitterly cold due to the Siberian High (often with winter temperatures comparable to their nearby subarctic climates), while summers are warm and long enough to avoid classification as a subarctic climate. In the Southern Hemisphere, it exists in well-defined areas only in the Southern Alps of New Zealand, in the Snowy Mountains of Australia in Kiandra, New South Wales and the Andes Mountains of Argentina and Chile. {{climate chart {{climate chart ==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. ==See also==