Jm. Paruelo et al., REGIONAL CLIMATIC SIMILARITIES IN THE TEMPERATE ZONES OF NORTH AND SOUTH-AMERICA, Journal of biogeography, 22(4-5), 1995, pp. 915-925
We performed an analysis of the climatic patterns of the temperate zon
es in North and South America using a global database of monthly preci
pitation and temperature. Three synthetic variables, identified by a p
rincipal component analysis (PCA) of the monthly data, were used: mean
annual precipitation, mean annual temperature and the proportion of t
he precipitation falling during summer. We displayed the spatial gradi
ent of the three variables by constructing a composite colour raster i
mage. We used a parallelepiped classification algorithm to locate area
s in both continents that are climatically similar to five North Ameri
can Long Term Ecological Research sites and to two South American long
-term ecological research sites. The same algorithm was used to identi
fy areas in South America which are climatically similar to some of th
e major grassland and shrubland types of North America. There is subst
antial overlap between the climates of North and South America. Most o
f the climatic patterns found in South America are well represented in
North America. However, there are certain climates in North America t
hat are not found in South America. An example is a climate with relat
ively low mean annual temperature and high summer precipitation. The c
limatic signatures of three North American LTER sites (Cedar Creek, CP
ER and Sevilleta) were not found in South America. The climatic signat
ures of two LTER sites (Konza and Jornada) had some representation in
South America. Two South American research sites (Rio Mayo and Las Chi
lcas) were well represented climatically in North America. The climate
s of six out of seven selected North American grassland and shrubland
types were represented in South America. The northern mixed prairie ty
pe was not represented climatically in South America. Our analysis sug
gests that comparisons of North and South America can provide a powerf
ul test of climatic control over vegetation.