Detecting and Modelling Regional Climate Change by Hans Alexandersson (auth.), Dr. Manola Brunet India, Dr.

By Hans Alexandersson (auth.), Dr. Manola Brunet India, Dr. Diego López Bonillo (eds.)

This special ebook, the 1st of its type, presents up to date, built-in and arranged, theoretical and methodological details on local weather switch and the linked environmental and socio-economic affects on a local scale. It offers the newest findings within the box of long term weather swap, which increase our knowing of the worldwide weather puzzle. Readers are brought to state of the art study in downscaling and GCMs. This contains the development of trustworthy local weather situations and the answer to key difficulties in regards to the assessmanet of the affects of weather switch within the most vital geographical parts on the earth: from Arctic to Antarctic areas, with particular emphasis at the Northern Hemisphere.

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________- L________ 1940 1960 ______ 1980 2000 Fig. 5. 4. 10 Part I: Quality Control Homogenisation Climate Time Series 6 ,-------,--------,-------,--------r-------,--------r-------, 5 4 3 2 o L-______ 1860 ~ ______- L_ _ _ _ _ _- J_ _ _ _ _ _ _ _L -_ _ _ _ _ _ 1880 1900 1920 1940 ~ _ _ _ _ _ _- L_ _ _ _ _ _ 1960 1980 ~ 2000 Fig. 6. Annual mean temperature (0C) in Sweden 1860-1999 based on lO homogenised series. identifies an increase of 12%. This is remarkable and corresponds to immense amounts of water.

1900 ! i .. . . . ~ ... ,.. ············ .. ·1··· . , i'-.... "-r: ..... ·······_·· .. 1: ......................... i ......................... 1....... ......................... ·r-::" ~ ,_/ 500 400 l~~- .............. 1.... i ... i j .. ·············1 ; .......................... ,! ________- L________ 1940 1960 ______ 1980 2000 Fig. 5. 4. 10 Part I: Quality Control Homogenisation Climate Time Series 6 ,-------,--------,-------,--------r-------,--------r-------, 5 4 3 2 o L-______ 1860 ~ ______- L_ _ _ _ _ _- J_ _ _ _ _ _ _ _L -_ _ _ _ _ _ 1880 1900 1920 1940 ~ _ _ _ _ _ _- L_ _ _ _ _ _ 1960 1980 ~ 2000 Fig.

Their number is increased by interpolated values for cases when the test could not detect inhomogeneities in individual months. For most stations some reasonable cause for the inhomogeneities detected by the statistical test could be found in the station history files. The dominant factor was the relocation of the stations. Especially those stations not run by meteorological service personnel but by engaged laymen and unpaid observers. These stations are often relocated so that the average undisturbed life time of the stations is not much more than 15 years.

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