Description Usage Arguments Value Formula References Examples
The Johansson Continentality Index is usually used for the climatic differentiation between continental and oceanic climates.
1 |
data |
daily mean temperature, Celsius |
data_names |
names of each period of time |
value |
lat |
na.rm |
logical. Should missing values (including NaN) be removed? |
... |
further arguments passed to or from other methods |
index value
JCI = \frac {1.7(Thm-Tcm)}{sinf}-20.4
Thm = Average temperature of the hottest month (Celsius); Tcm = Average temperature of the coldest month (Celsius); f = geographical latitude
Chronopoulou-Sereli A. 1996. Courses of Agricultural Meteorology.Publications Agricultural University of Athens: Athens, OH
1 2 |
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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 31.32472 27.70696
1982 1983 1984 1985 1986 1987 1988 1989
26.86611 28.94794 28.91290 33.27224 25.18493 30.11675 24.22669 26.38173
1990 1991 1992 1993 1994 1995 1996 1997
29.13463 30.71143 29.87391 25.49595 31.91680 24.58865 24.98971 23.97496
1998 1999 2000 2001 2002 2003 2004 2005
26.03217 27.25794 28.96622 32.39475 20.66315 32.98508 25.41399 33.54870
2006 2007 2008 2009 2010 2011 2012 2013
34.77385 25.21560 28.52877 33.98082 32.53374 30.46956 37.83580 29.79885
2014 2015 2016 2017
28.56872 37.35387 26.40859 32.17037
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