Typhoon turning atlas:
Gespeichert in:
1. Verfasser: | |
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Format: | Elektronisch E-Book |
Sprache: | English |
Veröffentlicht: |
Singapore ; Hackensack, NJ
World Scientific
[2014]
|
Schlagworte: | |
Online-Zugang: | FAW01 FAW02 Volltext |
Beschreibung: | Description based on print version record |
Beschreibung: | 1 online resource (viii, 441 pages) |
ISBN: | 9789814525190 9789814531818 9814525197 9814531812 |
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245 | 1 | 0 | |a Typhoon turning atlas |c Weihong Qian, Xiaolong Shan, Haoyuan Liang, Peking University, China |
264 | 1 | |a Singapore ; Hackensack, NJ |b World Scientific |c [2014] | |
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505 | 8 | |a Ch. 1. Variable decomposition. 1.1. Typhoons in the Northwest Pacific and the South China Sea. 1.2. Physical decomposition principles. 1.3. Statistical tracks. 1.4. Unusual motions of three typhoons. 1.5. Climatic monsoon troughs. 1.6. Two close tropical cyclones -- ch. 2. Typhoons without obvious turning motions. 2.1. Geneses in the South China Sea and the Philippines. 2.2. Intensity peaked in the South China Sea. 2.3. Intensity peaked in the Philippines. 2.4. Intensity peaked in the East Seas of China. 2.5. Intensity peaked in the Western Pacific -- ch. 3. Intensity peaked in the South China Sea. 3.1. Geneses in the South China Sea. 3.2. Geneses in the Philippines. 3.3. Geneses in the equatorial Pacific. 3.4. Geneses in the tropical Pacific -- ch. 4. Intensity peaked in the Philippines. 4.1. Geneses in the Philippines. 4.2. Geneses in the equatorial Western Pacific. 4.3. Geneses in the equatorial Central Pacific. 4.4. Geneses in the tropical Pacific -- ch. 5. Intensity peaked in the Taiwan area. 5.1. Geneses in the South China Sea . 5.2. Geneses in the Philippines. 5.3. Geneses in the equatorial Western Pacific. 5.4. Geneses in the equatorial Central Pacific. 5.5. Geneses in the tropical Western Pacific. 5.6. Geneses in the tropical Central Pacific -- ch. 6. Intensity peaked in the east seas of China. 6.1. Geneses in the equatorial Western Pacific. 6.2. Geneses in the equatorial Central Pacific. 6.3. Geneses in the tropical Western Pacific. 6.4. Geneses in the east seas of China. 6.5. Geneses in the Northwest Pacific -- ch. 7. Intensity peaked in the Pacific. 7.1. Intensity peaked in the equatorial Pacific. 7.2. Intensity peaked in the Northwest Pacific. 7.3. Geneses in the Western Pacific and entering the east seas of China. 7.4. Geneses in the Central Pacific and entering the East Seas ofChina. 7.5. Twin typhoons. 7.6. Complex tracks | |
505 | 8 | |a Typhoons with unusual tracks are difficult to forecast with respect to whether, when, and where typhoon turning occurs based on traditional synoptic charts and numerical weather forecast model products. This typhoon turning atlas provides an additional tool to deal with the typhoon turning question by using a physical decomposition method together with thousands of plots. In particular, this atlas provides important information of 322 historical typhoons that occurred in the past three decades and demonstrates how they were influenced respectively | |
650 | 7 | |a SCIENCE / Earth Sciences / Geography |2 bisacsh | |
650 | 7 | |a SCIENCE / Earth Sciences / Geology |2 bisacsh | |
650 | 7 | |a Cyclone forecasting |2 fast | |
650 | 7 | |a Decomposition method |2 fast | |
650 | 7 | |a Typhoons / Forecasting |2 fast | |
650 | 7 | |a Typhoons / Tracks |2 fast | |
650 | 4 | |a Geografie | |
650 | 4 | |a Geologie | |
650 | 4 | |a Geowissenschaften | |
650 | 4 | |a Typhoons |x Tracks |x Observations | |
650 | 4 | |a Typhoons |x Forecasting | |
650 | 4 | |a Cyclones |z Tropics |x Forecasting | |
650 | 4 | |a Decomposition method | |
700 | 1 | |a Shan, Xiaolong |e Sonstige |4 oth | |
700 | 1 | |a Liang, Haoyuan |e Sonstige |4 oth | |
776 | 0 | 8 | |i Erscheint auch als |n Druck-Ausgabe |a Qian, Weihong, author |t Typhoon turning atlas |
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author | Qian, Weihong |
author_facet | Qian, Weihong |
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building | Verbundindex |
bvnumber | BV043029138 |
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contents | Ch. 1. Variable decomposition. 1.1. Typhoons in the Northwest Pacific and the South China Sea. 1.2. Physical decomposition principles. 1.3. Statistical tracks. 1.4. Unusual motions of three typhoons. 1.5. Climatic monsoon troughs. 1.6. Two close tropical cyclones -- ch. 2. Typhoons without obvious turning motions. 2.1. Geneses in the South China Sea and the Philippines. 2.2. Intensity peaked in the South China Sea. 2.3. Intensity peaked in the Philippines. 2.4. Intensity peaked in the East Seas of China. 2.5. Intensity peaked in the Western Pacific -- ch. 3. Intensity peaked in the South China Sea. 3.1. Geneses in the South China Sea. 3.2. Geneses in the Philippines. 3.3. Geneses in the equatorial Pacific. 3.4. Geneses in the tropical Pacific -- ch. 4. Intensity peaked in the Philippines. 4.1. Geneses in the Philippines. 4.2. Geneses in the equatorial Western Pacific. 4.3. Geneses in the equatorial Central Pacific. 4.4. Geneses in the tropical Pacific -- ch. 5. Intensity peaked in the Taiwan area. 5.1. Geneses in the South China Sea . 5.2. Geneses in the Philippines. 5.3. Geneses in the equatorial Western Pacific. 5.4. Geneses in the equatorial Central Pacific. 5.5. Geneses in the tropical Western Pacific. 5.6. Geneses in the tropical Central Pacific -- ch. 6. Intensity peaked in the east seas of China. 6.1. Geneses in the equatorial Western Pacific. 6.2. Geneses in the equatorial Central Pacific. 6.3. Geneses in the tropical Western Pacific. 6.4. Geneses in the east seas of China. 6.5. Geneses in the Northwest Pacific -- ch. 7. Intensity peaked in the Pacific. 7.1. Intensity peaked in the equatorial Pacific. 7.2. Intensity peaked in the Northwest Pacific. 7.3. Geneses in the Western Pacific and entering the east seas of China. 7.4. Geneses in the Central Pacific and entering the East Seas ofChina. 7.5. Twin typhoons. 7.6. Complex tracks Typhoons with unusual tracks are difficult to forecast with respect to whether, when, and where typhoon turning occurs based on traditional synoptic charts and numerical weather forecast model products. This typhoon turning atlas provides an additional tool to deal with the typhoon turning question by using a physical decomposition method together with thousands of plots. In particular, this atlas provides important information of 322 historical typhoons that occurred in the past three decades and demonstrates how they were influenced respectively |
ctrlnum | (OCoLC)886540105 (DE-599)BVBBV043029138 |
dewey-full | 551.55/20916460223 |
dewey-hundreds | 500 - Natural sciences and mathematics |
dewey-ones | 551 - Geology, hydrology, meteorology |
dewey-raw | 551.55/20916460223 |
dewey-search | 551.55/20916460223 |
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dewey-tens | 550 - Earth sciences |
discipline | Geologie / Paläontologie |
format | Electronic eBook |
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id | DE-604.BV043029138 |
illustrated | Not Illustrated |
indexdate | 2024-07-10T07:15:26Z |
institution | BVB |
isbn | 9789814525190 9789814531818 9814525197 9814531812 |
language | English |
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physical | 1 online resource (viii, 441 pages) |
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publishDate | 2014 |
publishDateSearch | 2014 |
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publisher | World Scientific |
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spelling | Qian, Weihong Verfasser aut Typhoon turning atlas Weihong Qian, Xiaolong Shan, Haoyuan Liang, Peking University, China Singapore ; Hackensack, NJ World Scientific [2014] 1 online resource (viii, 441 pages) txt rdacontent c rdamedia cr rdacarrier Description based on print version record Ch. 1. Variable decomposition. 1.1. Typhoons in the Northwest Pacific and the South China Sea. 1.2. Physical decomposition principles. 1.3. Statistical tracks. 1.4. Unusual motions of three typhoons. 1.5. Climatic monsoon troughs. 1.6. Two close tropical cyclones -- ch. 2. Typhoons without obvious turning motions. 2.1. Geneses in the South China Sea and the Philippines. 2.2. Intensity peaked in the South China Sea. 2.3. Intensity peaked in the Philippines. 2.4. Intensity peaked in the East Seas of China. 2.5. Intensity peaked in the Western Pacific -- ch. 3. Intensity peaked in the South China Sea. 3.1. Geneses in the South China Sea. 3.2. Geneses in the Philippines. 3.3. Geneses in the equatorial Pacific. 3.4. Geneses in the tropical Pacific -- ch. 4. Intensity peaked in the Philippines. 4.1. Geneses in the Philippines. 4.2. Geneses in the equatorial Western Pacific. 4.3. Geneses in the equatorial Central Pacific. 4.4. Geneses in the tropical Pacific -- ch. 5. Intensity peaked in the Taiwan area. 5.1. Geneses in the South China Sea . 5.2. Geneses in the Philippines. 5.3. Geneses in the equatorial Western Pacific. 5.4. Geneses in the equatorial Central Pacific. 5.5. Geneses in the tropical Western Pacific. 5.6. Geneses in the tropical Central Pacific -- ch. 6. Intensity peaked in the east seas of China. 6.1. Geneses in the equatorial Western Pacific. 6.2. Geneses in the equatorial Central Pacific. 6.3. Geneses in the tropical Western Pacific. 6.4. Geneses in the east seas of China. 6.5. Geneses in the Northwest Pacific -- ch. 7. Intensity peaked in the Pacific. 7.1. Intensity peaked in the equatorial Pacific. 7.2. Intensity peaked in the Northwest Pacific. 7.3. Geneses in the Western Pacific and entering the east seas of China. 7.4. Geneses in the Central Pacific and entering the East Seas ofChina. 7.5. Twin typhoons. 7.6. Complex tracks Typhoons with unusual tracks are difficult to forecast with respect to whether, when, and where typhoon turning occurs based on traditional synoptic charts and numerical weather forecast model products. This typhoon turning atlas provides an additional tool to deal with the typhoon turning question by using a physical decomposition method together with thousands of plots. In particular, this atlas provides important information of 322 historical typhoons that occurred in the past three decades and demonstrates how they were influenced respectively SCIENCE / Earth Sciences / Geography bisacsh SCIENCE / Earth Sciences / Geology bisacsh Cyclone forecasting fast Decomposition method fast Typhoons / Forecasting fast Typhoons / Tracks fast Geografie Geologie Geowissenschaften Typhoons Tracks Observations Typhoons Forecasting Cyclones Tropics Forecasting Decomposition method Shan, Xiaolong Sonstige oth Liang, Haoyuan Sonstige oth Erscheint auch als Druck-Ausgabe Qian, Weihong, author Typhoon turning atlas http://search.ebscohost.com/login.aspx?direct=true&scope=site&db=nlebk&db=nlabk&AN=824735 Aggregator Volltext |
spellingShingle | Qian, Weihong Typhoon turning atlas Ch. 1. Variable decomposition. 1.1. Typhoons in the Northwest Pacific and the South China Sea. 1.2. Physical decomposition principles. 1.3. Statistical tracks. 1.4. Unusual motions of three typhoons. 1.5. Climatic monsoon troughs. 1.6. Two close tropical cyclones -- ch. 2. Typhoons without obvious turning motions. 2.1. Geneses in the South China Sea and the Philippines. 2.2. Intensity peaked in the South China Sea. 2.3. Intensity peaked in the Philippines. 2.4. Intensity peaked in the East Seas of China. 2.5. Intensity peaked in the Western Pacific -- ch. 3. Intensity peaked in the South China Sea. 3.1. Geneses in the South China Sea. 3.2. Geneses in the Philippines. 3.3. Geneses in the equatorial Pacific. 3.4. Geneses in the tropical Pacific -- ch. 4. Intensity peaked in the Philippines. 4.1. Geneses in the Philippines. 4.2. Geneses in the equatorial Western Pacific. 4.3. Geneses in the equatorial Central Pacific. 4.4. Geneses in the tropical Pacific -- ch. 5. Intensity peaked in the Taiwan area. 5.1. Geneses in the South China Sea . 5.2. Geneses in the Philippines. 5.3. Geneses in the equatorial Western Pacific. 5.4. Geneses in the equatorial Central Pacific. 5.5. Geneses in the tropical Western Pacific. 5.6. Geneses in the tropical Central Pacific -- ch. 6. Intensity peaked in the east seas of China. 6.1. Geneses in the equatorial Western Pacific. 6.2. Geneses in the equatorial Central Pacific. 6.3. Geneses in the tropical Western Pacific. 6.4. Geneses in the east seas of China. 6.5. Geneses in the Northwest Pacific -- ch. 7. Intensity peaked in the Pacific. 7.1. Intensity peaked in the equatorial Pacific. 7.2. Intensity peaked in the Northwest Pacific. 7.3. Geneses in the Western Pacific and entering the east seas of China. 7.4. Geneses in the Central Pacific and entering the East Seas ofChina. 7.5. Twin typhoons. 7.6. Complex tracks Typhoons with unusual tracks are difficult to forecast with respect to whether, when, and where typhoon turning occurs based on traditional synoptic charts and numerical weather forecast model products. This typhoon turning atlas provides an additional tool to deal with the typhoon turning question by using a physical decomposition method together with thousands of plots. In particular, this atlas provides important information of 322 historical typhoons that occurred in the past three decades and demonstrates how they were influenced respectively SCIENCE / Earth Sciences / Geography bisacsh SCIENCE / Earth Sciences / Geology bisacsh Cyclone forecasting fast Decomposition method fast Typhoons / Forecasting fast Typhoons / Tracks fast Geografie Geologie Geowissenschaften Typhoons Tracks Observations Typhoons Forecasting Cyclones Tropics Forecasting Decomposition method |
title | Typhoon turning atlas |
title_auth | Typhoon turning atlas |
title_exact_search | Typhoon turning atlas |
title_full | Typhoon turning atlas Weihong Qian, Xiaolong Shan, Haoyuan Liang, Peking University, China |
title_fullStr | Typhoon turning atlas Weihong Qian, Xiaolong Shan, Haoyuan Liang, Peking University, China |
title_full_unstemmed | Typhoon turning atlas Weihong Qian, Xiaolong Shan, Haoyuan Liang, Peking University, China |
title_short | Typhoon turning atlas |
title_sort | typhoon turning atlas |
topic | SCIENCE / Earth Sciences / Geography bisacsh SCIENCE / Earth Sciences / Geology bisacsh Cyclone forecasting fast Decomposition method fast Typhoons / Forecasting fast Typhoons / Tracks fast Geografie Geologie Geowissenschaften Typhoons Tracks Observations Typhoons Forecasting Cyclones Tropics Forecasting Decomposition method |
topic_facet | SCIENCE / Earth Sciences / Geography SCIENCE / Earth Sciences / Geology Cyclone forecasting Decomposition method Typhoons / Forecasting Typhoons / Tracks Geografie Geologie Geowissenschaften Typhoons Tracks Observations Typhoons Forecasting Cyclones Tropics Forecasting |
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