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43-548: Columbia City is the name of several places in the United States: Columbia City, Indiana Columbia City, Oregon Columbia City, Seattle , a neighborhood of Seattle See also [ edit ] Columbia (disambiguation) Columbia, Missouri Columbia, South Carolina [REDACTED] Topics referred to by the same term This disambiguation page lists articles about distinct geographical locations with

86-655: 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 very small parts of the Intermountain West in the United States. This climate zone does not exist at all in the Southern Hemisphere, where

129-607: A classification). More extreme and inland humid continental climates, sometimes known as "hyper-continental" climates, are found in northeast China , southern Siberia , Mongolia , Kazakhstan , most of the southern interior of Canada , and the Upper Midwest , where temperatures in the winter resemble those of adjacent subarctic climates (with long, drier, generally very cold winters) but have longer and generally warmer summers (in occasional cases, hot summers). A more moderate variety, found in places like Honshu , east-central China,

172-510: A male householder with no wife present, and 38.9% were non-families. 33.5% of all households were made up of individuals, and 14.2% had someone living alone who was 65 years of age or older. The average household size was 2.32 and the average family size was 2.93. The median age in the city was 36.1 years. 24.9% of residents were under the age of 18; 9.1% were between the ages of 18 and 24; 26.7% were from 25 to 44; 23.9% were from 45 to 64; and 15.3% were 65 years of age or older. The gender makeup of

215-509: 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 and Asia an occasional tropical cyclone (or

258-704: 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 . 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

301-523: 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 700 m (2,297 ft)), Poland , Czech Republic , Slovakia , Hungary (generally above 100 m (328 ft)), Croatia (mostly Slavonia region), in much of Eastern Europe : Ukraine (the whole country except

344-445: Is 25 miles away from Fort Wayne, 20 miles away from Warsaw, and 69 miles away from South Bend, making it a strategic location for business. As of the census of 2010, there were 8,750 people, 3,658 households, and 2,235 families residing in the city. The population density was 1,568.1 inhabitants per square mile (605.4/km ). There were 3,944 housing units at an average density of 706.8 per square mile (272.9/km ). The racial makeup of

387-592: Is a city in Columbia Township, Whitley County, Indiana , United States. The population was 9,892 at the 2020 Census , up from 8,750 at the 2010 Census , estimated to be 10,064 in 2023. The city is the county seat of Whitley County, and is the largest community therein. It is part of the Fort Wayne MSA . The first non-Native American settlers arrived in 1837 as a result of the end of the Black Hawk War and

430-619: Is elected in a citywide vote, along with the city councilperson-at-large. The remaining four council members are elected from individual city districts: northeast, southeast, southwest and northwest. There is also a city clerk-treasurer who is elected in a citywide vote. The Columbia City post office has been in operation since 1854. The town has a lending library, the Peabody Public Library. Hot-summer humid continental climate Humid continental climates are generally found between latitudes 40° N and 60° N , within

473-510: 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

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516-463: Is less extreme than the most inland hyper-continental variety. Using the Köppen climate classification , a climate is classified as humid continental when the temperature of the coldest month is below 0 °C [32.0 °F] or −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,

559-554: Is less seasonally uniform in the west. The western states of the western United States (namely Montana , Wyoming , parts of southern Idaho , most of Lincoln County in Eastern Washington , parts of Colorado , parts of Utah , isolated parts of northern New Mexico , 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

602-714: Is noted during the autumn of deciduous forests. 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

645-689: Is to be found in northern China including Manchuria and parts of North China , south-east 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

688-682: 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 ), Denmark , Finland (south end, including the three largest cities ), Norway (most populated area), all Baltic States : Estonia , Latvia , Lithuania and also in parts of: Romania (generally above 100 m (328 ft)), Bosnia and Herzegovina , Turkey and in

731-473: The Cairngorm Mountains of Scotland , (generally above 100 m (328 ft)). 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 Asia, this climate type

774-473: 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 to the effects of

817-524: The Korean Peninsula , parts of Eastern Europe , parts of southern Ontario , much of the American Midwest , and the Northeast US , the climate combines hotter summer maxima and greater humidity (similar to those found in adjacent humid subtropical climates ) and moderately cold winters and more intermittent snow cover (averaging somewhat below freezing, too cold for a more temperate classification), and

860-543: The 2010 census, Columbia City has a total area of 5.601 square miles (14.51 km ), of which 5.58 square miles (14.45 km ) (or 99.63%) is land and 0.021 square miles (0.05 km ) (or 0.37%) is water. According to the Köppen Climate Classification system, Columbia City has a hot-summer humid continental climate , abbreviated "Dfa" on climate maps. The hottest temperature recorded in Columbia City

903-574: The Canadian Prairie Provinces 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

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946-693: The Erie Canal. They were from New England - "Yankee" Settlers, descendants of the English Puritans who settled New England in the colonial era. They were primarily members of the Congregational Church though due to the Second Great Awakening many of them had converted to Methodism and some had become Baptists before coming to what is now Columbia City. Columbia City was founded in 1839, originally just being called "Columbia". The name

989-529: The Western United States) grade into semi-arid climates with similar temperatures but low precipitation. 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

1032-403: The average family size was 2.89. In the city, the population was spread out, with 24.4% under the age of 18, 9.9% from 18 to 24, 29.1% from 25 to 44, 18.8% from 45 to 64, and 17.7% who were 65 years of age or older. The median age was 36 years. For every 100 females, there were 89.2 males. For every 100 females age 18 and over, there were 85.8 males. The median income for a household in the city

1075-420: The central and northeastern portions of North America , Europe , and Asia . Occasionally, they can also be found at higher elevations above other more temperate climate types. They are rare in the Southern Hemisphere , limited to isolated high altitude locations, due to the larger ocean area at that latitude, smaller land mass, and the consequent greater maritime moderation. In the Northern Hemisphere, some of

1118-565: The city was 47.6% male and 52.4% female. As of the census of 2000, there were 7,077 people, 3,018 households, and 1,874 residing in the city. The population density was 1,359.5 inhabitants per square mile (524.9/km ). There were 3,191 housing units at an average density of 613.0 per square mile (236.7/km ). The racial makeup of the city was 98.11% White , 0.32% African American , 0.44% Native American , 0.08% Asian , 0.03% Pacific Islander , 0.34% from other races , and 0.68% from two or more races. Hispanic or Latino of any race were 1.20% of

1161-420: The city was 96.7% White , 0.5% African American , 0.3% Native American , 0.5% Asian , 0.6% from other races , and 1.4% from two or more races. Hispanic or Latino of any race were 2.2% of the population. There were 3,658 households, of which 30.9% had children under the age of 18 living with them, 42.4% were married couples living together, 13.9% had a female householder with no husband present, 4.8% had

1204-453: The classification symbol defines seasonal rainfall as follows: while the third letter denotes the extent of summer heat: Within North America, moisture within this climate regime is supplied by the Great Lakes , 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

1247-425: 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. Also known as hemiboreal climate , areas featuring this subtype of the continental climate have an average temperature in

1290-514: 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. Within North America , this climate includes portions of the central and eastern United States from east of 100°W to south of about the 44°N to the Atlantic . Precipitation increases further eastward in this zone and

1333-439: The humid continental climate covers a much larger area than the hot subtype. In North America, the climate zone covers from about 42°N to 50°N latitude mostly east of 100°W , including parts of Southern Ontario , the southern half of Quebec , The Maritimes , and Newfoundland , as well as the northern United States from eastern North Dakota east to Maine . However, it can be found as far north as 54°N , and further west in

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1376-470: The humid continental climates, typically in around Hokkaido , Sakhalin Island , northeastern mainland Europe , Scandinavia , Nova Scotia , and Newfoundland are closer to the sea and heavily maritime-influenced and comparable to oceanic climates , with relatively cool summers, significant year-round precipitation (including high amounts of snow) and winters being just below the freezing mark (too cold for such

1419-559: The population would have tripled. Columbia City was incorporated in the state of Indiana in 1888. The Whitley County Courthouse was designed (1888–1891) by Brentwood S. Tolan , of Fort Wayne, Indiana. The building was added to the National Register of Historic Places in 1979. The Thomas R. Marshall House was added to the register in 1983 and the Columbia City Historic District was added in 1987. According to

1462-409: The population. There were 3,018 households, out of which 30.6% had children under the age of 18 living with them, 45.8% were married couples living together, 12.4% had a female householder with no husband present, and 37.9% were non-families. 33.6% of all households were made up of individuals, and 15.1% had someone living alone who was 65 years of age or older. The average household size was 2.27 and

1505-537: The remnants thereof). 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 . By definition, forests thrive within this climate. Biomes within this climate regime include temperate woodlands, temperate grasslands, temperate deciduous or evergreen forests, coniferous forests, and coniferous swamps. Within wetter areas, maple , spruce , pine , fir , and oak can be found. Fall foliage

1548-481: The same name. If an internal link led you here, you may wish to change the link to point directly to the intended article. Retrieved from " https://en.wikipedia.org/w/index.php?title=Columbia_City&oldid=1063023126 " Category : Place name disambiguation pages Hidden categories: Short description is different from Wikidata All article disambiguation pages All disambiguation pages Columbia City, Indiana Columbia City

1591-573: The steppe ( BSk ) climates. In the eastern and Midwestern United States, Pennsylvania , Ohio , Illinois , Indiana , southern New York , most of Connecticut and Rhode Island , and eastern Massachusetts fall into the hot-summer humid continental climate. In Canada, this climate type exists only over portions of Southern Ontario . In the Eastern Hemisphere, this climate regime is found within interior Eurasia and east-central Asia. Within Europe,

1634-488: 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 , between Tokyo and Hokkaidō and 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

1677-435: The warmest month below 22 °C (72 °F). 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 well or far below the −3 °C (27 °F) (or 0 °C (32.0 °F)) isotherm. Frost-free periods typically last 3–5 months. Heat spells lasting over a week are rare. The warm summer version of

1720-455: The −3 °C (27 °F) average temperature isotherm (line of equal temperature) was near the southern extent of winter snowpack . In the United States, it is more common to use the 0 °C [32.0 °F] isotherm instead. The 10 °C (50 °F) average temperature was found to be roughly the minimum temperature necessary for tree reproduction and growth. Wide temperature ranges are common within this climate zone. Second letter in

1763-411: Was $ 36,112, and the median income for a family was $ 47,357. Males had a median income of $ 34,803 versus $ 21,740 for females. The per capita income for the city was $ 19,296. About 4.5% of families and 6.4% of the population were below the poverty line , including 5.8% of those under age 18 and 9.8% of those age 65 or over. The city government consists of a mayor and a five-member city council. The mayor

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1806-626: Was 103 °F (39.4 °C) on June 26, 1988, while the coldest temperature recorded was −24 °F (−31.1 °C) on January 19–21, 1994. About 12 percent of Columbia City's population is employed in the manufacturing sector. This makes it one of the most important sectors in the city. Currently there are 6 businesses employing 50 - 350 people in the city. Those six companies are 80/20, Coupled Products, LLC, Alcoils, inc., Reelcraft Industries, Inc. ChromaSource, Inc. and Kilgore Manufacturing Company, Inc. The city also has agricultural roots with it contributing heavily to its economy. Columbia City

1849-468: Was later changed in 1854 since there was already a city named Columbia in the state. Many public debates were held to discuss different names for the city, but it was later only reduced to two: "Beaver" and "Columbia City." Eventually, the name Columbia City was selected. The completion of the Pittsburgh, Fort Wayne, & Chicago Railway in 1856 brought rapid growth to the small town, and from 1865 to 1875

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