HISTORY Lecture Notes - Lecture 27: International Date Line, Landfall, Japan Meteorological Agency

8 views2 pages

Document Summary

El ni o is the warm period of the el ni o southern oscillation (enso) and is related with a band of warm sea water that creates in the focal and east-focal tropical pacific (roughly between the. International date line and 120 w), including the region off the pacific bank of south america. Enso is the pattern of warm and cold ocean surface temperature (sst) of the tropical focal and eastern pacific ocean. El ni o is joined by high pneumatic stress in the western pacific and low gaseous tension in the eastern pacific. El ni o stages are known to endure near four years; nonetheless, records show that the cycles have kept going somewhere in the range of two and seven years. During the advancement of el ni o, precipitation creates between september november. The cool period of enso is spanish: la ni a, lit.

Get access

Grade+
$40 USD/m
Billed monthly
Grade+
Homework Help
Study Guides
Textbook Solutions
Class Notes
Textbook Notes
Booster Class
10 Verified Answers
Class+
$30 USD/m
Billed monthly
Class+
Homework Help
Study Guides
Textbook Solutions
Class Notes
Textbook Notes
Booster Class
7 Verified Answers

Related Documents

Related Questions