Titre :	Climate - Diagram maps of the individual continents and the ecological climatic regions of the earth: supplement to the vegetation monographs
Type de document :	texte imprimé
Auteurs :	Walter, H. ; Harnickell, E. ; Mueller - Dombois, D.
Mention d'édition :	Springer - verlag Berlin
Editeur :	Springer - Verlag Berlin
Année de publication :	1975
ISBN/ISSN/EAN :	CI-10945
Note générale :	The climat - diagram maps contained in this volume are to serve for a quick orientation of the cliamte and its zonation in the various world regions. The climate - diagram maps have several advantages over the usual climatic zonation maps. There are: 1) they show the transitory changes between the individual climate types, 2) there is no need of any interpolation or convension of the climatic data, and 3) the climate types are clearly shown in the form of diagrams. This facilitates the detection of homochimates, i.e., stations with closely similar climates.
Langues :	Anglais (eng)
Mots-clés :	Climatologie  Ecologie  Oscillation climatique  Zonage  Cartographie  Diagramme climatologique
Index. décimale :	577 Ecologie
Résumé :	The climat - diagram maps contained in this volume are to serve for a quick orientation of the cliamte and its zonation in the various world regions. The climate - diagram maps have several advantages over the usual climatic zonation maps. There are: 1) they show the transitory changes between the individual climate types, 2) there is no need of any interpolation or convension of the climatic data, and 3) the climate types are clearly shown in the form of diagrams. This facilitates the detection of homochimates, i.e., stations with closely similar climates.
Note de contenu :	The climat - diagram maps contained in this volume are to serve for a quick orientation of the cliamte and its zonation in the various world regions. The climate - diagram maps have several advantages over the usual climatic zonation maps. There are: 1) they show the transitory changes between the individual climate types, 2) there is no need of any interpolation or convension of the climatic data, and 3) the climate types are clearly shown in the form of diagrams. This facilitates the detection of homochimates, i.e., stations with closely similar climates.

Climate - Diagram maps of the individual continents and the ecological climatic regions of the earth: supplement to the vegetation monographs [texte imprimé] / Walter, H. ; Harnickell, E. ; Mueller - Dombois, D.  . -  Springer - verlag Berlin . - Springer - Verlag Berlin, 1975.
ISSN : CI-10945
The climat - diagram maps contained in this volume are to serve for a quick orientation of the cliamte and its zonation in the various world regions. The climate - diagram maps have several advantages over the usual climatic zonation maps. There are: 1) they show the transitory changes between the individual climate types, 2) there is no need of any interpolation or convension of the climatic data, and 3) the climate types are clearly shown in the form of diagrams. This facilitates the detection of homochimates, i.e., stations with closely similar climates.
Langues : Anglais (eng)

Mots-clés :	Climatologie  Ecologie  Oscillation climatique  Zonage  Cartographie  Diagramme climatologique
Index. décimale :	577 Ecologie
Résumé :	The climat - diagram maps contained in this volume are to serve for a quick orientation of the cliamte and its zonation in the various world regions. The climate - diagram maps have several advantages over the usual climatic zonation maps. There are: 1) they show the transitory changes between the individual climate types, 2) there is no need of any interpolation or convension of the climatic data, and 3) the climate types are clearly shown in the form of diagrams. This facilitates the detection of homochimates, i.e., stations with closely similar climates.
Note de contenu :	The climat - diagram maps contained in this volume are to serve for a quick orientation of the cliamte and its zonation in the various world regions. The climate - diagram maps have several advantages over the usual climatic zonation maps. There are: 1) they show the transitory changes between the individual climate types, 2) there is no need of any interpolation or convension of the climatic data, and 3) the climate types are clearly shown in the form of diagrams. This facilitates the detection of homochimates, i.e., stations with closely similar climates.