Climate
The climate is the weather averaged over a long period of time. In a given geographical region, the climate generally does not vary over time on the scale of a human life span. However, over geological time, climate can vary considerably for a given place on the earth. For example, Scandinavia has been through a number of ice ages over hundreds of thousands of years (the last one ending about 10,000 years ago). Paleoclimatology is the study of these past climates.
Climate is a concept used to divide the world into regions sharing similar climatic parameters. Climate regions can be classified on the basis of temperature and precipitation alone — one of the most popular methods of climate classification is that developed by Vladimir Köppen:
Köppen's climate classification scheme
- GROUP A - Tropical climates: Tropical
climates (see tropics)
are characterized by constant high temperature - all twelve
months of the year have average temperatures of 18 °C
(64.4 °F) or higher. They are subdivided as follows:
- Af (Equatorial) climate: - all twelve
months have average precipitation above 60 mm. These
climates, usually occurring within 5° latitude
of the equator, are dominated by the Doldrums Low
Pressure all year round, and thus have no seasons.
Examples: - Singapore; Manaus, Brazil. - Am (Tropical monsoon) climate: This type
of climate, found chiefly in southern Asia,
results from the monsoon
winds which switch direction according to the seasons.
This climate has a driest month with rainfall less
than 60 mm, but more than (100 - (total annual precipitation/25)):
Examples: Mumbai, India; Rangoon, Burma - Aw (Tropical wet and dry) climate - these
climates have a pronounced dry season, with the driest
month having precipitation less than (100 - (total
annual precipitation (mm)/25)) mm:
Examples: Kayes, Mali; Parana, Brazil
- Af (Equatorial) climate: - all twelve
months have average precipitation above 60 mm. These
climates, usually occurring within 5° latitude
of the equator, are dominated by the Doldrums Low
Pressure all year round, and thus have no seasons.
- GROUP B - Arid climates: These climates
are characterized by the fact that precipitation is less
than evaporation. The threshold is determined as follows:
- To find the precipitation threshold (in millimetres), multiply the average annual temperature in °C by 20, then add 280 (if 70%+ precipitation is in warmest 6 months) or 140 (if 30%-70% precipitation is in warmest 6 months).
- If the annual precipitation is less than half the threshold for Group B, it is classified as BW (desert climate) - if it is less than the threshold but more than half the threshold, it is classified as BS (semi-desert climate).
- A third letter can be added to indicate temperature: h signifies hot climate (average annual temperature above 18 °C), while k signifies temperate climate (average annual temperature below 18 °C).
- Examples: In Salah, Algeria
(BWh)
Chimbai, Uzbekistan (BWk)
Gaborone, Botswana (BSh)
Astrakhan, Russia (BSk)
- GROUP C - Warm temperate climates:
These climates have an average temperature above 10 °C
(50 °F) in their warmest months, and a coldest month
average between -3 °C and 18 °C.
- The second letter indicates the precipitation pattern - w indicates dry winters (driest winter month average precipitation less than one-tenth wettest summer month average precipitation), s inidicates dry summers (driest summer month less than 30 mm average precipitation, and less than one-third wettest winter month precipitation) and f means rain in all seasons (neither above mentioned condition fulfilled).
- The third letter indicates the degree of summer heat - a indicates warmest month average temperature above 22 °C, b indicates warmest month average temperature below 22 °C, with at least 4 months averaging above 10 °C, while c means 3 or fewer months with mean temperatures above 10 °C.
- Group C climates may be divided as follows:
- Mediterranean climates (Csa,
Csb) - these climates usually occur on
the western sides of continents between the latitudes
of 30° and 45°. These climates are in
the polar front region in winter, and thus have
moderate temperatures and changeable weather.
Summers are hot and dry, due to the domination
of the subtropical high pressure systems.
Examples: Lisbon, Portugal (Csa)
Athens, Greece (Csa)
Santiago, Chile (Csb)
San Francisco, California (Csb) - Humid Subtropical climates
(Cfa, Cwa) - these climates
usually occur in the interiors of continents,
or on their east coasts, between the latitudes
of 25° and 40°. Unlike the Mediterranean
climates, the summers are humid due to unstable
tropical air masses, or onshore Trade Winds. In
mainland Asia,
winters are sometimes dry, due to monsoonal influence.
Examples: Memphis, Tennessee (Cfa)
Buenos Aires, Argentina (Cfa)
New Delhi, India (Cwa)
Tokyo, Japan (Cfa). - Maritime Temperate climates
(Cfb) - these climates usually occur
on the western sides of continents between the
latitudes of 45° and 55°. These climates
are dominated all year round by the polar front,
leading to changeable, often overcast weather.
Summers are cool due to cloud cover, but winters
are milder than other climates in similar latitudes.
Examples: London, England
Vancouver, British Columbia
Valdivia, Chile
Christchurch, New Zealand. - Maritime Subarctic climates
(Cfc) - these climates occur poleward
of the Maritime Temperate climates.
Examples: Ushuaia, Argentina
Torshavn, Faroes
- Mediterranean climates (Csa,
Csb) - these climates usually occur on
the western sides of continents between the latitudes
of 30° and 45°. These climates are in
the polar front region in winter, and thus have
moderate temperatures and changeable weather.
Summers are hot and dry, due to the domination
of the subtropical high pressure systems.
- GROUP D - Continental climates: These
climates have an average temperature above 10 °C in
their warmest months, and a coldest month average below
-3 °C. These usually occur in the interiors of continents,
or on their east coasts, north of 40° North latitude.
Group D climates do not exist at all in the Southern hemisphere
due to the smaller land masses here.
- The second and third letters are used as for Group C climates, while a third letter of d indicates 3 or fewer months with mean temperatures above 10 °C, and a coldest month temperature below -38 °C.
- Group D climates may be divided as follows:
- Hot Summer Continental climates
(Dfa, Dwa) - these climates
usually occur in the forties latitudes. In mainland
Asia,
winters are sometimes dry due to monsoonal influence.
Examples: Chicago, Illinois (Dfa)
Beijing, China (Dwa). - Cool Summer Continental climates
(Dfb, Dwb) - these climates
are immediately north of Hot Summer Continental
climates, and also in central and eastern Europe,
between the Maritime Temperate and Continental
Subarctic climates.
Examples: Montreal, Quebec (Dfb)
Warsaw, Poland (Dfb)
Vladivostok, Russia (Dwb) - Continental Subarctic climates
(Dfc, Dwc, Dfd) - these
climates occur poleward of the other Group D climates,
mostly north of 50° North latitude.
Examples: Schefferville, Quebec
Yakutsk, Russia
- Hot Summer Continental climates
(Dfa, Dwa) - these climates
usually occur in the forties latitudes. In mainland
Asia,
winters are sometimes dry due to monsoonal influence.
- GROUP E - Polar climates: These climates
are characterized by average temperatures below 10 °C
in all twelve months of the year:
- ET (Tundra) climate: - warmest month has
an average temperature between 0 °C and 10 °C.
These climates occur on the northern edges of the
North American and Eurasian landmasses.
Examples: - Point Barrow, Alaska
Norilsk, Russia
Svalbard, Norway. - EF (Ice Cap) climate: - all twelve months
have average temperatures below 0 °C. This climates
is dominant in Antarctica and in inland Greenland.
- ET (Tundra) climate: - warmest month has
an average temperature between 0 °C and 10 °C.
These climates occur on the northern edges of the
North American and Eurasian landmasses.