You are here -allRefer - Reference - Country Study & Country Guide - China >

allRefer Reference and Encyclopedia Resource

allRefer    
allRefer
   


-- Country Study & Guide --     

 

China

 
Country Guide
Afghanistan
Albania
Algeria
Angola
Armenia
Austria
Azerbaijan
Bahrain
Bangladesh
Belarus
Belize
Bhutan
Bolivia
Brazil
Bulgaria
Cambodia
Chad
Chile
China
Colombia
Caribbean Islands
Comoros
Cyprus
Czechoslovakia
Dominican Republic
Ecuador
Egypt
El Salvador
Estonia
Ethiopia
Finland
Georgia
Germany
Germany (East)
Ghana
Guyana
Haiti
Honduras
Hungary
India
Indonesia
Iran
Iraq
Israel
Cote d'Ivoire
Japan
Jordan
Kazakhstan
Kuwait
Kyrgyzstan
Latvia
Laos
Lebanon
Libya
Lithuania
Macau
Madagascar
Maldives
Mauritania
Mauritius
Mexico
Moldova
Mongolia
Nepal
Nicaragua
Nigeria
North Korea
Oman
Pakistan
Panama
Paraguay
Peru
Philippines
Poland
Portugal
Qatar
Romania
Russia
Saudi Arabia
Seychelles
Singapore
Somalia
South Africa
South Korea
Soviet Union [USSR]
Spain
Sri Lanka
Sudan
Syria
Tajikistan
Thailand
Turkmenistan
Turkey
Uganda
United Arab Emirates
Uruguay
Uzbekistan
Venezuela
Vietnam
Yugoslavia
Zaire

China

Climate

Monsoon winds, caused by differences in the heat-absorbing capacity of the continent and the ocean, dominate the climate. Alternating seasonal air-mass movements and accompanying winds are moist in summer and dry in winter. The advance and retreat of the monsoons account in large degree for the timing of the rainy season and the amount of rainfall throughout the country. Tremendous differences in latitude, longitude, and altitude give rise to sharp variations in precipitation and temperature within China. Although most of the country lies in the temperate belt, its climatic patterns are complex.

China's northernmost point lies along the Heilong Jiang in Heilongjiang Province in the cold-temperate zone; its southernmost point, Hainan Island, has a tropical climate (see table 4, Appendix A). Temperature differences in winter are great, but in summer the diversity is considerably less. For example, the northern portions of Heilongjiang Province experience an average January mean temperature of below 0°C, and the reading may drop to minus 30°C; the average July mean in the same area may exceed 20°C. By contrast, the central and southern parts of Guangdong Province experience an average January temperature of above 10°C, while the July mean is about 28°C.

Precipitation varies regionally even more than temperature. China south of the Qin Ling experiences abundant rainfall, most of it coming with the summer monsoons. To the north and west of the range, however, rainfall is uncertain. The farther north and west one moves, the scantier and more uncertain it becomes. The northwest has the lowest annual rainfall in the country and no precipitation at all in its desert areas.

Data as of July 1987


China - TABLE OF CONTENTS

  • China - Physical Environment and Population

  • China -The Social System

  • China - Education and Culture


  • Go Up - Top of Page

    Make allRefer Reference your HomepageAdd allRefer Reference to your FavoritesGo to Top of PagePrint this PageSend this Page to a Friend


    Information Courtesy: The Library of Congress - Country Studies


    Content on this web site is provided for informational purposes only. We accept no responsibility for any loss, injury or inconvenience sustained by any person resulting from information published on this site. We encourage you to verify any critical information with the relevant authorities.

     

     

     
     


    About Us | Contact Us | Terms of Use | Privacy | Links Directory
    Link to allRefer | Add allRefer Search to your site

    ©allRefer
    All Rights reserved. Site best viewed in 800 x 600 resolution.