Description Usage Arguments Value Formula References Examples
De Martonne aridity index is the ratio between the annual amount of precipitation and anual mean of temperature plus 10 Celsius.
1 |
pr |
daily precipitation, mm |
taverage |
daily mean temperature, Celsius |
data_names |
names of each period of time |
na.rm |
logical. Should missing values (including NaN) be removed? |
... |
further arguments passed to or from other methods |
index value
MAI = \frac{P} {TG+10}
P = annual precipitation (mm); TG = mean annual air temperature (Celsius)
De Martonne E., 1926. Une nouvelle fonction climatologique: L’indice d’aridité. La Meteorologie, 449-458.
1 2 |
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# Package SPEI (1.7) loaded [try SPEINews()].
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2050 2051 2052 2053 2054 2055 2056 2057
NA NA NA NA NA NA NA NA
2058 2059 2060 2061 2062 2063 2064 2065
NA NA NA NA NA NA NA NA
2066 2067 2068 1969 1970 1971 1972 1973
NA NA NA NA NA NA NA NA
1974 1975 1976 1977 1978 1979 1980 1981
NA NA NA NA NA NA 24.41496 22.20308
1982 1983 1984 1985 1986 1987 1988 1989
25.77840 21.38974 25.79232 21.30028 26.01198 25.52069 26.15076 29.92953
1990 1991 1992 1993 1994 1995 1996 1997
19.71477 24.14550 23.73315 20.49254 14.18020 19.86997 29.47697 25.57808
1998 1999 2000 2001 2002 2003 2004 2005
20.90682 20.92114 17.24457 16.18496 25.58041 25.38202 21.46937 17.39997
2006 2007 2008 2009 2010 2011 2012 2013
17.36177 21.48162 29.10595 19.28905 27.19403 19.43908 17.77395 26.33624
2014 2015 2016 2017
21.33112 20.96459 22.81382 15.70575
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