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| http://dbpedia.org/ontology/abstract | The climate of the United States varies du … The climate of the United States varies due to changes in latitude, and a range of geographic features, including mountains and deserts. Generally, on the mainland, the climate of the U.S. becomes warmer the further south one travels, and drier the further west, until one reaches the West Coast. West of 100°W, much of the U.S. has a cold semi-arid climate in the interior upper western states (Idaho to the Dakotas), to warm to hot desert and semi-arid climates in the southwestern U.S. East of 100°W, the climate is humid continental in northern areas (locations roughly above 40°N, Northern Plains, Midwest, Great Lakes, New England), transitioning into a humid temperate climate from the Southern Plains and lower Midwest east to the Middle Atlantic states (Virginia to southern Connecticut). A humid subtropical climate is found along and south of a mostly east–west line from the Virginia/Maryland capes (north of the greater Norfolk, Virginia area), westward to approximately northern Oklahoma, north of the greater Oklahoma City area. Along the Atlantic seaboard, the humid subtropical climate zone extends southward into central Florida. A Mediterranean climate prevails along most of the California coast, while southern Florida has a tropical climate, the warmest region on the US mainland. Hawaii and the U.S. territories also have tropical climates. Higher-elevation areas of the Rocky Mountains, the Wasatch Range, Sierra Nevada, and Cascade Range are alpine. Coastal areas of Oregon and Washington have an oceanic climate. The state of Alaska, on the northwestern corner of the North American continent, is largely dominated by a subarctic climate, but with a subpolar oceanic climate in the southeast (Alaska Panhandle), southwestern peninsula and Aleutian Islands, and a polar climate in the north. The primary drivers of weather in the contiguous United States are the seasonal change in the solar angle, the migration north–south of the subtropical highs, and the seasonal change in the position of the polar jet stream. In the Northern Hemisphere summer, the subtropical high pressure systems move northward and closer to the United States mainland. In the Atlantic Ocean, the Bermuda High creates a south-southwest flow of tropical air masses over the southeastern, south-central and central United States – resulting in warm to hot temperatures, high humidity and frequent intense (but usually brief) showers and/or thunderstorms as the heat builds in the afternoon. In the Northern Hemisphere summer, high pressure in the Pacific Ocean builds toward the California coast, resulting in a northwesterly airflow, creating the cool, dry, and stable weather conditions prevalent along the West Coast in summer. In the Northern Hemisphere winter, the subtropical highs retreat southward. The polar jet stream (and associated conflict zone between cold, dry air masses from Canada and warm, moist air masses from the Gulf of Mexico) drops further southward into the United States – bringing more frequent periods of stormy weather, with rain, ice and snow, and much more variable temperatures, with rapid temperature rises and falls not uncommon. Areas in the southern U.S. (Florida, the Gulf Coast, the Desert Southwest, and southern California) however, often have more stable weather, as the polar jet stream's impact does not usually reach that far south. Weather systems, be they high-pressure systems (anticyclones), low-pressure systems (cyclones) or fronts (boundaries between air masses of differing temperature, humidity and most commonly, both) are faster-moving and more intense in the winter/colder months than in the summer/warmer months, when the belt of lows and storms generally moves into southern Canada. The Gulf of Alaska is the origination area of many storms that enter the United States. Such "North Pacific lows" enter the U.S. through the Pacific Northwest, then move eastward across the northern Rocky Mountains, northern Great Plains, upper Midwest, Great Lakes and New England states. Across the central states from late fall to spring, "Panhandle hook" storms move from the central Rockies into the Oklahoma/Texas panhandle areas, then northeast toward the Great Lakes. They generate unusually large temperature contrasts, and often bring copious Gulf moisture northward, resulting sometimes in cold conditions and possibly-heavy snow or ice north and west of the storm track, and warm conditions, heavy rains and potentially-severe thunderstorms south and east of the storm track – often simultaneously. Across the northern states in winter usually from Montana eastward, "Alberta clipper" storms track east and bring light to moderate snowfalls from Montana and the Dakotas across the upper Midwest and Great Lakes states to New England, and often, windy and severe Arctic outbreaks behind them. When winter-season Canadian cold air masses drop unusually far southward, "Gulf lows" can develop in or near the Gulf of Mexico, then track eastward or northeastward across the Southern states, or nearby Gulf or South Atlantic waters. They sometimes bring rain, but can bring snow or ice across the South, mostly in interior or northern areas. In the cold season (generally November to March), most precipitation occurs in conjunction with organized low-pressure systems and associated fronts. In the summer, storms are much more localized, with short-duration thunderstorms common in many areas east of 100°W and south of 40°N. In the warm season, storm systems affecting a large area are less frequent, and weather conditions are more solar {sun} controlled, with the greatest chance for thunderstorm and severe weather activity during peak heating hours, mostly between 3 PM and 9 PM local time. From May to August especially, often-overnight mesoscale-convective-system (MCS) thunderstorm complexes, usually associated with frontal activity, can deliver significant to flooding rainfall amounts from the Dakotas/Nebraska eastward across Iowa/Minnesota to the Great Lakes states. From late summer into fall (mostly August to October), tropical cyclones (hurricanes, tropical storms and tropical depressions) sometimes approach or cross the Gulf and Atlantic states, bringing high winds, heavy rainfall, and storm surges (often topped with battering waves) to Gulf and Atlantic lowlands and coastal areas.f and Atlantic lowlands and coastal areas. , Podnebí Spojených států amerických je velm … Podnebí Spojených států amerických je velmi různorodé. Obzvláště celá střední část USA je náchylná k extrémním výkyvům počasí, protože je zde od Karibiku po Severní Dakotu rovina, a tak nic nebrání prudkým přesunům větrů ze severu na jih a naopak. Západní pobřeží se zase vyznačuje mírnějším počasím, které je ale směrem na jih od Seattlu sušší a teplejší. Naopak na východním pobřeží mohou být zimy dost studené. Největrnější je středozápad, což je hluboké vnitrozemí, průměrná roční rychlost větru je tam 5-6 m/s, jinak na většině území je to mezi 2,5 až 4 m/s. Nejméně větrná oblast je východní Kalifornie, kde je to 2 m/s.[zdroj?!] Amplituda průměrných měsíčních teplot v roce (rozdíl mezi průměrnou měsíční teplotou nejchladnějšího a nejteplejšího měsíce) je od 10 °C v teplotně nejstálejších oblastech na západním pobřeží až po 35 °C v těch teplotně nejméně stálých hluboko ve vnitrozemí. Teplotně nejstálejší je však Havaj, kde je kvůli tropickému podnebí tento rozdíl jen 4 °C. tropickému podnebí tento rozdíl jen 4 °C. , Das Klima der Vereinigten Staaten ist äußerst vielfältig. Es herrschen mehrere Klimazonen vor, wie z. B. das kontinentale, subtropische, mediterrane sowie im südlichen Florida tropische Klima. , Il clima degli Stati Uniti d'America, data … Il clima degli Stati Uniti d'America, data la vastità del territorio, presenta una grande varietà. La zona nordorientale subisce l'afflusso di aria fredda ed è caratterizzata da inverni freddi e piogge abbondanti. La zona degli Appalachi ha un clima montano, più umido sul versante est, ventoso a ovest, in direzione delle Grandi Pianure. Le Montagne Rocciose hanno un clima montano. Le pianure interne sono aride, con temperature estive elevatissime in alcune regioni. Il clima della costa del Pacifico, riscaldata dalla Corrente della California, è mite e piovoso a nord, e diventa più caldo scendendo verso sud, fino al clima semi-desertico al confine con il Messico. semi-desertico al confine con il Messico. , Сполу́чені Шта́ти Аме́рики розташовані в р … Сполу́чені Шта́ти Аме́рики розташовані в різних кліматичних умовах. Територія розсічена горами, що простягаються з півночі на південь, країна незахищена з півночі й півдня. Найбільша температура у Сполучених Штатах Америки спостерігається в Долині Смерті. Деколи температура піднімається там до 56 градусів вище нуля за Цельсієм. там до 56 градусів вище нуля за Цельсієм. , Cet article concerne les différents types de climat aux États-Unis. , Из-за большого размера страны, её протяжён … Из-за большого размера страны, её протяжённости и широкого разнообразия географических особенностей на территории США можно найти районы с практически любыми климатическими характеристиками. Бо́льшая часть США (северная и центральная часть США) располагается в зоне умеренного климата, в южной части США преобладает субтропический климат, Гавайи и южная часть Флориды лежат в зоне тропиков, север Аляски относится к полярным регионам, а в остальной части Аляски преобладает субарктический климат. Великие равнины к западу от 100-го меридиана относят к полупустыням, Большой Бассейн и области вокруг него имеют аридный, а прибрежные районы Калифорнии — средиземноморский климат. Тип климата в границах одного пояса может существенно меняться в зависимости от рельефа, близости океана и других факторов. Благоприятный климат оказал немалое влияние на заселение материка европейцами и во многом способствовал занятию США лидирующих позиций в мире.вал занятию США лидирующих позиций в мире. , 由於幅員遼闊和众多的地理特徵，美國幾乎有着世界上所有的氣候類型： * 东北部沿海和 … 由於幅員遼闊和众多的地理特徵，美國幾乎有着世界上所有的氣候類型： * 东北部沿海和五大湖区属柯本氣候分類法的“”或周淑貞氣候分類法的溫帶大陸性濕潤氣候：受拉布拉多寒流和南下冷空气影响，冬季较冷，夏季较温和，多雨雪，年平均降雨量1000毫米左右； * 东南部和墨西哥湾沿岸属于“”或周淑貞氣候分類法的副熱帶濕潤氣候：受墨西哥湾暖流影响，温暖湿润，年降雨量2000毫米以上； * 中部平原：寒暖气流均可长驱直入，夏季炎热，冬季寒冷多雪； * 西部内陆高原：冬季干燥寒冷，夏季干燥炎热，年降雨量500毫米以下； * 西部太平洋沿岸：南段属“亚热带地中海型气候”，北段属“”或周淑貞氣候分類法的溫帶海洋性氣候。 影響美國氣候的主要是北極氣流，每年從太平洋帶來大規模的低氣壓，這些低氣壓在通過內華達山脈、洛磯山脈、和喀斯喀特山脈時夾帶大量水分，當這些氣壓到達中部大平原時便能進行重組，導致主要的氣團相遇而帶來激烈的大雷雨，尤其是在春季和夏季。有時這些暴雨可能與其他的低氣壓會合，繼續前往東海岸和大西洋，並會演變為更激烈的東北風暴（Nor'easter），在美國東北的中大西洋區域和新英格蘭形成廣泛而沉重的降雪。大平原廣闊無比的草原也形成許多世界上最極端的氣候轉變現象。 大盆地地區和哥伦比亚高原則是乾旱而極少降雨的地區，最乾旱時平均降雨量少於38毫米。美國西南部是乾旱的沙漠，夏季時最熱的數個禮拜溫度超過38℃。西南部和大盆地地區也會受到來自加利福尼亞灣的季风影響，偶爾會帶來少見的大雨。加利福尼亞州大多數區域都屬於地中海式气候，有時會在每年的10月至隔年的4月引發強烈豪雨，而其他月份幾乎全無降雨。瀕臨太平洋的西北方地區則終年豪雨不斷，但在冬季和春季降雨量最大。西部山脈吸收充足的濕氣，降雨量和降雪都相當沉重。喀斯喀特山脈是世界上降雪量最多的地方之一，但海拔較低的沿海地區降雪不多。 近年來由於全球暖化導致的持續性氣候變遷，包括加利福尼亞州、內華達州、亞利桑那州與數個其餘州在內的西部地區自2011年開始發生連續四年的嚴重乾旱，降雪量降至僅僅平均百分之六的歷史新低，導致水庫儲水量大幅削減，同時也導致加利福尼亞州農業灌溉與民用水源的大幅度限制。加利福尼亞州更是在2015年4月1日宣布該州有史以來首個大幅減少用水量百分之二十五的行政命令。州更是在2015年4月1日宣布該州有史以來首個大幅減少用水量百分之二十五的行政命令。 |
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| http://dbpedia.org/property/aprHighF | 64.4 |
| http://dbpedia.org/property/aprLowF | 39.3 |
| http://dbpedia.org/property/aprPrecipitationInch | 2.7 |
| http://dbpedia.org/property/aprRecordHighF | 118 |
| http://dbpedia.org/property/aprRecordLowF | −50 |
| http://dbpedia.org/property/augHighF | 85.8 |
| http://dbpedia.org/property/augLowF | 60.3 |
| http://dbpedia.org/property/augPrecipitationInch | 2.68 |
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| http://dbpedia.org/property/caption | In recent decades, record high daily temperatures have predominated over record daily low temperatures, with record daily highs now numbering more than twice that of record daily lows. , The 20-year average of the number of annual Category 4 and 5 hurricanes in the Atlantic region has approximately doubled since the year 2000. |
| http://dbpedia.org/property/date | November 2011 |
| http://dbpedia.org/property/decHighF | 44.2 |
| http://dbpedia.org/property/decLowF | 24.4 |
| http://dbpedia.org/property/decPrecipitationInch | 2.51 |
| http://dbpedia.org/property/decRecordHighF | 100 |
| http://dbpedia.org/property/decRecordLowF | −72 |
| http://dbpedia.org/property/febHighF | 46.5 |
| http://dbpedia.org/property/febLowF | 24.8 |
| http://dbpedia.org/property/febPrecipitationInch | 2.14 |
| http://dbpedia.org/property/febRecordHighF | 105 |
| http://dbpedia.org/property/febRecordLowF | −75 |
| http://dbpedia.org/property/image | 1920.0 , 1980 |
| http://dbpedia.org/property/janHighF | 42.6 |
| http://dbpedia.org/property/janLowF | 22.2 |
| http://dbpedia.org/property/janPrecipitationInch | 2.34 |
| http://dbpedia.org/property/janRecordHighF | 101 |
| http://dbpedia.org/property/janRecordLowF | −80 |
| http://dbpedia.org/property/julHighF | 87.1 |
| http://dbpedia.org/property/julLowF | 61.7 |
| http://dbpedia.org/property/julPrecipitationInch | 2.85 |
| http://dbpedia.org/property/julRecordHighF | 134 |
| http://dbpedia.org/property/julRecordLowF | 8 |
| http://dbpedia.org/property/junHighF | 82.1 |
| http://dbpedia.org/property/junLowF | 56.9 |
| http://dbpedia.org/property/junPrecipitationInch | 3.11 |
| http://dbpedia.org/property/junRecordHighF | 129 |
| http://dbpedia.org/property/junRecordLowF | -11 |
| http://dbpedia.org/property/location | Contiguous US average , United States |
| http://dbpedia.org/property/marHighF | 55.3 |
| http://dbpedia.org/property/marLowF | 31.9 |
| http://dbpedia.org/property/marPrecipitationInch | 2.53 |
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| http://dbpedia.org/property/marRecordLowF | −68 |
| http://dbpedia.org/property/mayHighF | 73.6 |
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| http://dbpedia.org/property/mayPrecipitationInch | 3.09 |
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| http://dbpedia.org/property/mayRecordLowF | −25 |
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| http://dbpedia.org/property/novRecordLowF | −62 |
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| http://dbpedia.org/property/octLowF | 42.2 |
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| http://dbpedia.org/property/octRecordLowF | −45 |
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| http://dbpedia.org/property/sepLowF | 53.2 |
| http://dbpedia.org/property/sepPrecipitationInch | 2.56 |
| http://dbpedia.org/property/sepRecordHighF | 126 |
| http://dbpedia.org/property/sepRecordLowF | −15 |
| http://dbpedia.org/property/singleLine | yes , Yes |
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| rdfs:comment | Il clima degli Stati Uniti d'America, data … Il clima degli Stati Uniti d'America, data la vastità del territorio, presenta una grande varietà. La zona nordorientale subisce l'afflusso di aria fredda ed è caratterizzata da inverni freddi e piogge abbondanti. La zona degli Appalachi ha un clima montano, più umido sul versante est, ventoso a ovest, in direzione delle Grandi Pianure. Le Montagne Rocciose hanno un clima montano. Le pianure interne sono aride, con temperature estive elevatissime in alcune regioni. Il clima della costa del Pacifico, riscaldata dalla Corrente della California, è mite e piovoso a nord, e diventa più caldo scendendo verso sud, fino al clima semi-desertico al confine con il Messico. semi-desertico al confine con il Messico. , Сполу́чені Шта́ти Аме́рики розташовані в р … Сполу́чені Шта́ти Аме́рики розташовані в різних кліматичних умовах. Територія розсічена горами, що простягаються з півночі на південь, країна незахищена з півночі й півдня. Найбільша температура у Сполучених Штатах Америки спостерігається в Долині Смерті. Деколи температура піднімається там до 56 градусів вище нуля за Цельсієм. там до 56 градусів вище нуля за Цельсієм. , Das Klima der Vereinigten Staaten ist äußerst vielfältig. Es herrschen mehrere Klimazonen vor, wie z. B. das kontinentale, subtropische, mediterrane sowie im südlichen Florida tropische Klima. , Cet article concerne les différents types de climat aux États-Unis. , Из-за большого размера страны, её протяжён … Из-за большого размера страны, её протяжённости и широкого разнообразия географических особенностей на территории США можно найти районы с практически любыми климатическими характеристиками. Бо́льшая часть США (северная и центральная часть США) располагается в зоне умеренного климата, в южной части США преобладает субтропический климат, Гавайи и южная часть Флориды лежат в зоне тропиков, север Аляски относится к полярным регионам, а в остальной части Аляски преобладает субарктический климат. Великие равнины к западу от 100-го меридиана относят к полупустыням, Большой Бассейн и области вокруг него имеют аридный, а прибрежные районы Калифорнии — средиземноморский климат. Тип климата в границах одного пояса может существенно меняться в зависимости от рельефа, близости океана и других фактороврельефа, близости океана и других факторов , 由於幅員遼闊和众多的地理特徵，美國幾乎有着世界上所有的氣候類型： * 东北部沿海和 … 由於幅員遼闊和众多的地理特徵，美國幾乎有着世界上所有的氣候類型： * 东北部沿海和五大湖区属柯本氣候分類法的“”或周淑貞氣候分類法的溫帶大陸性濕潤氣候：受拉布拉多寒流和南下冷空气影响，冬季较冷，夏季较温和，多雨雪，年平均降雨量1000毫米左右； * 东南部和墨西哥湾沿岸属于“”或周淑貞氣候分類法的副熱帶濕潤氣候：受墨西哥湾暖流影响，温暖湿润，年降雨量2000毫米以上； * 中部平原：寒暖气流均可长驱直入，夏季炎热，冬季寒冷多雪； * 西部内陆高原：冬季干燥寒冷，夏季干燥炎热，年降雨量500毫米以下； * 西部太平洋沿岸：南段属“亚热带地中海型气候”，北段属“”或周淑貞氣候分類法的溫帶海洋性氣候。 影響美國氣候的主要是北極氣流，每年從太平洋帶來大規模的低氣壓，這些低氣壓在通過內華達山脈、洛磯山脈、和喀斯喀特山脈時夾帶大量水分，當這些氣壓到達中部大平原時便能進行重組，導致主要的氣團相遇而帶來激烈的大雷雨，尤其是在春季和夏季。有時這些暴雨可能與其他的低氣壓會合，繼續前往東海岸和大西洋，並會演變為更激烈的東北風暴（Nor'easter），在美國東北的中大西洋區域和新英格蘭形成廣泛而沉重的降雪。大平原廣闊無比的草原也形成許多世界上最極端的氣候轉變現象。格蘭形成廣泛而沉重的降雪。大平原廣闊無比的草原也形成許多世界上最極端的氣候轉變現象。 , The climate of the United States varies du … The climate of the United States varies due to changes in latitude, and a range of geographic features, including mountains and deserts. Generally, on the mainland, the climate of the U.S. becomes warmer the further south one travels, and drier the further west, until one reaches the West Coast. The primary drivers of weather in the contiguous United States are the seasonal change in the solar angle, the migration north–south of the subtropical highs, and the seasonal change in the position of the polar jet stream.e in the position of the polar jet stream. , Podnebí Spojených států amerických je velm … Podnebí Spojených států amerických je velmi různorodé. Obzvláště celá střední část USA je náchylná k extrémním výkyvům počasí, protože je zde od Karibiku po Severní Dakotu rovina, a tak nic nebrání prudkým přesunům větrů ze severu na jih a naopak. Západní pobřeží se zase vyznačuje mírnějším počasím, které je ale směrem na jih od Seattlu sušší a teplejší. Naopak na východním pobřeží mohou být zimy dost studené. Největrnější je středozápad, což je hluboké vnitrozemí, průměrná roční rychlost větru je tam 5-6 m/s, jinak na většině území je to mezi 2,5 až 4 m/s. Nejméně větrná oblast je východní Kalifornie, kde je to 2 m/s.[zdroj?!] Amplituda průměrných měsíčních teplot v roce (rozdíl mezi průměrnou měsíční teplotou nejchladnějšího a nejteplejšího měsíce) je od 10 °C v teplotně nejstálejších obe) je od 10 °C v teplotně nejstálejších ob |
| rdfs:label | Клімат США , Clima degli Stati Uniti d'America , Климат США , Iklim Amerika Serikat , Podnebí Spojených států amerických , 美國氣候 , Climate of the United States , Climat des États-Unis , Klima der Vereinigten Staaten |
| rdfs:seeAlso | http://dbpedia.org/resource/United_States_rainfall_climatology + , http://dbpedia.org/resource/American_Samoa + |
| hide properties that link here |
