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건조 기후 둘러보기 메뉴eh00564958문서를 완성해

열대 우림열대 몬순사바나열대 하계 소우온난 습윤서안 해양성온대 하우지중해성툰드라빙설


기후


사막 기후스텝 기후












건조 기후




위키백과, 우리 모두의 백과사전.






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건조 기후(乾燥氣候)는 일반적으로 연평균 강수량이 500mm 미만이라고 정의하지만 독일의 지리학자 쾨펜(Wladimir Peter Köppen, 1846~1940)은 연평균 강수량이 연평균 기온과 강수의 계절적분포의 상관관계로 성립된 건조한계에 이르지 못하였을때를 건조 기후라 정의하였다. 주로 아열대 고압대, 남, 북위 30도대와 수분이 부족한 대륙 내부 그리고 한류가 흘러들어가는 대륙 서안에 위치한다. 건조 기후는 사막 기후와 스텝 기후로 나누어지는데, 이 역시 일반적으로 연평균 강수량 250mm를 기준으로 나누지만, 쾨펜은 건조한계의 1/2인 사막한계를 기준으로 구분하였다.







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