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Climate is the long-term pattern of weather in an area, typically averaged over a period of 30 years.[1][2] More rigorously, it is the mean and variability of meteorological variables over a time spanning from months to millions of years.[1] Some of the meteorological variables that are commonly measured are temperature, humidity, atmospheric pressure, wind, and precipitation. In a broader sense, climate is the state of the components of the climate system, which includes the ocean, land, and ice on Earth.[1] The climate of a location is affected by its latitude/longitude, terrain, and altitude, as well as nearby water bodies and their currents. Climates can be classified according to the average and the typical ranges of different variables, most commonly temperature and precipitation. The most commonly used classification scheme was the Köppen climate classification. The Thornthwaite system,[3] in use since 1948, incorporates evapotranspiration along with temperature and precipitation information and is used in studying biological diversity and how climate change affects it. The Bergeron and Spatial Synoptic Classification systems focus on the origin of air masses that define the climate of a region. Paleoclimatology is the study of ancient climates. Since very few direct observations of climate are available before the 19th century, paleoclimates are inferred from proxy variables that include non-biotic evidence such as sediments found in lake beds and ice cores, and biotic evidence such as tree rings and coral. Climate models are mathematical models of past, present and future climates. Climate change may occur over long and short timescales from a variety of factors; recent warming is discussed in global warming. Global warming results in redistributions. For example, "a 3°C change in mean annual temperature corresponds to a shift in isotherms of approximately 300–400 km in latitude (in the temperate zone) or 500 m in elevation. Therefore, species are expected to move upwards in elevation or towards the poles in latitude in response to shifting climate zones"

INTO JAPANESE

気候は、ある地域の長期的な気象パターンであり、通常は30年間の平均です。[1] [2]より厳密には、それは数ヶ月から数百万年にわたる期間にわたる気象変数の平均と変動性です。[1]一般的に測定される気象変数のいくつかは、温度、湿度、大気プレスです

BACK INTO ENGLISH

Climate is a long-term weather pattern in a region, usually a 30-year average. [1] [2] More precisely, it is the mean and variability of meteorological variables over a period of months to millions of years. [1] Some of the commonly measured meteorological variables are temperature, humidity, and atmospheric press.

INTO JAPANESE

気候は地域の長期的な気象パターンであり、通常は30年の平均です。 [1] [2]より正確には、それは数ヶ月から数百万年の期間にわたる気象変数の平均と変動性です。 [1]一般的に測定される気象変数には、気温、湿度、大気圧などがあります。

BACK INTO ENGLISH

Climate is a long-term weather pattern in the region, usually a 30-year average. [1] [2] More precisely, it is the mean and variability of meteorological variables over a period of months to millions of years. [1] Commonly measured meteorological variables include temperature, humidity, and atmospheric pressure.

INTO JAPANESE

気候はこの地域の長期的な気象パターンであり、通常は30年の平均です。 [1] [2]より正確には、それは数ヶ月から数百万年の期間にわたる気象変数の平均と変動性です。 [1]一般的に測定される気象変数には、温度、湿度、大気圧などがあります。

BACK INTO ENGLISH

Climate is a long-term weather pattern in the region, usually a 30-year average. [1] [2] More precisely, it is the mean and variability of meteorological variables over a period of months to millions of years. [1] Commonly measured meteorological variables include temperature, humidity, and atmospheric pressure.