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Climate Atlas of Eurasian and North American Arctic regions

by Christian Momberger
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Current price ₹2,157.00
Original price ₹2,499.00
Original price ₹2,499.00
Original price ₹2,499.00
(-14%)
₹2,157.00
Current price ₹2,157.00

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Book cover type: Paperback
  • ISBN13: 9783640135356
  • Binding: Paperback
  • Subject: N/A
  • Publisher: Grin Verlag
  • Publisher Imprint: Grin Verlag
  • Publication Date:
  • Pages: 68
  • Original Price: USD 25.5
  • Language: English
  • Edition: N/A
  • Item Weight: 100 grams
  • BISAC Subject(s): Earth Sciences / Geography

Research Paper (undergraduate) from the year 2001 in the subject Geography / Earth Science - Physical Geography, Geomorphology, Environmental Studies, grade: 1,7, University of Lapland (Arctic Center), course: Ecological and Historical Biogeography of Arctic and Alpine Regions, language: English, abstract: The present climate atlas will show the climatic differences between selected arctic regions from Eurasia, or strictly speaking Russia, and North America. The main emphasis will thereby be put on the difference between oceanic (maritime) and continental climate. It will also show the spread of permafrost and the localisation of the Arctic tree line, which both depends on the existing climate. In the Appendix, the climate-diagrams for each selected station and equivalent maps of the chosen sections and for the locating of the tree line and the permafrost can be found. ------------------------------------------------------------------ Der hier vorliegende Klima-Atlas zeigt die klimatischen Unterschiede zwischen ausgewählten Arktischen Region in Eurasien (Russland) und Nordamerika. Der Schwerpunkt wird dabei auf die Unterschiede zwischen maritimen und kontinentalen Klima gelegt. Im Klima-Atlas wird aber auch auf die Verbreitung der Permafrostgebiete und den Verlauf der arktischen Baumgrenze eingegangen. Im Anhang finden man die Klimadiagramme für jede ausgewählte Klimastation und entsprechende Karten für die gewählten Sektionen sowie zur Verbreitung des Permafrosts und dem Verlauf der arktischen Baumgrenze.

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