East Asian monsoon:
The East Asian summer monsoon has complex space and time structures that are distinct from the South Asian summer monsoon. It covers both subtropics and midlatitudes and its rainfall tends to be concentrated in rain belts that stretch for many thousands of kilometers and affect China, Japan, Korea,...
Gespeichert in:
| Format: | Elektronisch E-Book |
|---|---|
| Sprache: | English |
| Veröffentlicht: |
Singapore
World Scientific Pub. Co.
c2004
|
| Schlagworte: | |
| Online-Zugang: | FHN01 Volltext |
| Zusammenfassung: | The East Asian summer monsoon has complex space and time structures that are distinct from the South Asian summer monsoon. It covers both subtropics and midlatitudes and its rainfall tends to be concentrated in rain belts that stretch for many thousands of kilometers and affect China, Japan, Korea, and the surrounding areas. The circulation of the East Asian winter monsoon encompasses a large meridional domain with cold air outbreaks emanating from the Siberian high and penetrates deeply into the equatorial Maritime Continent region, where the center of maximum rainfall has long been recognized as a major planetary scale heat source that provides a significant amount of energy which drives the global circulation during boreal winter. The East Asian summer monsoon is also closely linked with the West Pacific summer monsoon. Both are part of the global climate system and are affected by El Nino-Southern Oscillation (ENSO) and surface temperature variations in the western Pacific and surrounding oceans, the tropospheric biennial oscillation, and the South Asian summer monsoon. In addition, typhoons in the western North Pacific are most active during the East Asian summer monsoon. They may be considered as a component of the East Asian summer monsoon as they contribute substantial amounts of rainfall and have major impacts on the region. Because of its impacts on nearly one-third of the world's population and on the global climate system (including effects on the climate change), the study of the East Asian monsoon has received increased attention both in East Asian countries and in the United States. This book presents reviews of recent research on the subject |
| Beschreibung: | viii, 564 p. ill. (some col.), maps (some col.) |
| ISBN: | 9789812701411 |
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| 520 | |a The East Asian summer monsoon has complex space and time structures that are distinct from the South Asian summer monsoon. It covers both subtropics and midlatitudes and its rainfall tends to be concentrated in rain belts that stretch for many thousands of kilometers and affect China, Japan, Korea, and the surrounding areas. The circulation of the East Asian winter monsoon encompasses a large meridional domain with cold air outbreaks emanating from the Siberian high and penetrates deeply into the equatorial Maritime Continent region, where the center of maximum rainfall has long been recognized as a major planetary scale heat source that provides a significant amount of energy which drives the global circulation during boreal winter. The East Asian summer monsoon is also closely linked with the West Pacific summer monsoon. Both are part of the global climate system and are affected by El Nino-Southern Oscillation (ENSO) and surface temperature variations in the western Pacific and surrounding oceans, the tropospheric biennial oscillation, and the South Asian summer monsoon. In addition, typhoons in the western North Pacific are most active during the East Asian summer monsoon. They may be considered as a component of the East Asian summer monsoon as they contribute substantial amounts of rainfall and have major impacts on the region. Because of its impacts on nearly one-third of the world's population and on the global climate system (including effects on the climate change), the study of the East Asian monsoon has received increased attention both in East Asian countries and in the United States. This book presents reviews of recent research on the subject | ||
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| spelling | East Asian monsoon edited by C.-P. Chang Singapore World Scientific Pub. Co. c2004 viii, 564 p. ill. (some col.), maps (some col.) txt rdacontent c rdamedia cr rdacarrier The East Asian summer monsoon has complex space and time structures that are distinct from the South Asian summer monsoon. It covers both subtropics and midlatitudes and its rainfall tends to be concentrated in rain belts that stretch for many thousands of kilometers and affect China, Japan, Korea, and the surrounding areas. The circulation of the East Asian winter monsoon encompasses a large meridional domain with cold air outbreaks emanating from the Siberian high and penetrates deeply into the equatorial Maritime Continent region, where the center of maximum rainfall has long been recognized as a major planetary scale heat source that provides a significant amount of energy which drives the global circulation during boreal winter. The East Asian summer monsoon is also closely linked with the West Pacific summer monsoon. Both are part of the global climate system and are affected by El Nino-Southern Oscillation (ENSO) and surface temperature variations in the western Pacific and surrounding oceans, the tropospheric biennial oscillation, and the South Asian summer monsoon. In addition, typhoons in the western North Pacific are most active during the East Asian summer monsoon. They may be considered as a component of the East Asian summer monsoon as they contribute substantial amounts of rainfall and have major impacts on the region. Because of its impacts on nearly one-third of the world's population and on the global climate system (including effects on the climate change), the study of the East Asian monsoon has received increased attention both in East Asian countries and in the United States. This book presents reviews of recent research on the subject Monsoons / East Asia Winds / East Asia Monsun (DE-588)4170491-5 gnd rswk-swf Ostasien (DE-588)4075727-4 gnd rswk-swf 1\p (DE-588)4143413-4 Aufsatzsammlung gnd-content Ostasien (DE-588)4075727-4 g Monsun (DE-588)4170491-5 s 2\p DE-604 Chang, C.-P. Sonstige oth Erscheint auch als Druck-Ausgabe 9789812387691 Erscheint auch als Druck-Ausgabe 9812387692 http://www.worldscientific.com/worldscibooks/10.1142/5482#t=toc Verlag URL des Erstveroeffentlichers Volltext 1\p cgwrk 20201028 DE-101 https://d-nb.info/provenance/plan#cgwrk 2\p cgwrk 20201028 DE-101 https://d-nb.info/provenance/plan#cgwrk |
| spellingShingle | East Asian monsoon Monsoons / East Asia Winds / East Asia Monsun (DE-588)4170491-5 gnd |
| subject_GND | (DE-588)4170491-5 (DE-588)4075727-4 (DE-588)4143413-4 |
| title | East Asian monsoon |
| title_auth | East Asian monsoon |
| title_exact_search | East Asian monsoon |
| title_full | East Asian monsoon edited by C.-P. Chang |
| title_fullStr | East Asian monsoon edited by C.-P. Chang |
| title_full_unstemmed | East Asian monsoon edited by C.-P. Chang |
| title_short | East Asian monsoon |
| title_sort | east asian monsoon |
| topic | Monsoons / East Asia Winds / East Asia Monsun (DE-588)4170491-5 gnd |
| topic_facet | Monsoons / East Asia Winds / East Asia Monsun Ostasien Aufsatzsammlung |
| url | http://www.worldscientific.com/worldscibooks/10.1142/5482#t=toc |
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