Debundscha

Last updated
Debundscha
Village
Cameroon adm location map.svg
Red pog.svg
Debundscha
Coordinates: 4°6′N8°59′E / 4.100°N 8.983°E / 4.100; 8.983
CountryFlag of Cameroon.svg  Cameroon
RegionSouthwest Region
DivisionFako
Elevation
36 m (118 ft)
Time zone UTC+1 (WAT)
Climate Af

Debundscha is a village in the south-western Region of the republic of Cameroon. It is found at the foot of the Mount Cameroon at its south western corner directly facing the south Atlantic Ocean on the Cameroon coast.

Contents

Debundscha has an extremely wet climate with about 10,299 millimetres (405.5 in) of rainfall falling annually. [1]

The village of Debundscha is included among the five rainiest places in the world which includes Lloró, Mawsynram, the Big Bog and Cherrapunji, with each of them receiving over 10,000 millimeters (400 inches) of rain annually. [2]

History

The Germans installed a lighthouse in Debundscha in 1904. [3] [4]

Climate

Its proximity to the equator which is consistently hot and humid, gives Debundscha a long rainy season and a short dry season in a year. Debundscha's coastal location with the giant Mount Cameroon behind it, a giant mountain massive rising from the coast of the South Atlantic ocean to a height of about 4,095 metres (13,435 ft) [5] and blocking rain forming clouds from passing it results in abundant rainfall for Debundscha during the year.

The major rainfall falls on the ocean-facing south-western slope of Mount Cameroon and on Debundscha, at the foot of this slope. [6] [7]

Climate data for Debundscha
MonthJanFebMarAprMayJunJulAugSepOctNovDecYear
Mean daily maximum °C (°F)29.5
(85.1)
29.9
(85.8)
30.0
(86.0)
30.0
(86.0)
29.9
(85.8)
28.8
(83.8)
27.6
(81.7)
27.2
(81.0)
27.6
(81.7)
27.6
(81.7)
28.6
(83.5)
29.1
(84.4)
28.8
(83.9)
Daily mean °C (°F)25.8
(78.4)
26.5
(79.7)
26.6
(79.9)
26.7
(80.1)
26.5
(79.7)
25.7
(78.3)
24.7
(76.5)
24.6
(76.3)
24.8
(76.6)
24.6
(76.3)
25.7
(78.3)
25.5
(77.9)
25.6
(78.2)
Mean daily minimum °C (°F)22.1
(71.8)
23.1
(73.6)
23.1
(73.6)
23.3
(73.9)
23.1
(73.6)
22.6
(72.7)
21.8
(71.2)
22.0
(71.6)
22.1
(71.8)
21.6
(70.9)
22.8
(73.0)
22.0
(71.6)
22.5
(72.4)
Average rainfall mm (inches)153
(6.0)
298
(11.7)
371
(14.6)
476
(18.7)
604
(23.8)
1,093
(43.0)
1,413
(55.6)
1,623
(63.9)
1,325
(52.2)
1,144
(45.0)
413
(16.3)
177
(7.0)
9,090
(357.8)
Mean monthly sunshine hours 147.3143.7122.3118.4119.489.161.535.452.867.999.4130.81,188
Source: [8]

See also

Related Research Articles

<span class="mw-page-title-main">Geography of Cameroon</span>

At 475,440 km2 (183,570 sq mi), Cameroon is the world's 53rd largest country. It is slightly larger than the nation of Sweden and the US state of California. It is comparable in size to Papua New Guinea. Cameroon's landmass is 472,710 km2 (182,510 sq mi), with 2,730 km2 (1,050 sq mi) of water.

<span class="mw-page-title-main">Geography of Cape Verde</span>

Cape Verde is a group of arid Atlantic islands which are home to distinct communities of plants, birds, and reptiles. The islands constitute the unique Cape Verde Islands dry forests ecoregion, according to the World Wildlife Fund.

<span class="mw-page-title-main">Geography of Nicaragua</span>

Nicaragua is a country in Central America, bordering both the Caribbean Sea and the North Pacific Ocean, between Costa Rica and Honduras. Nicaragua is the largest country in Central America in square kilometers.

<span class="mw-page-title-main">Geography of Spain</span>

Spain is a country located in southwestern Europe occupying most of the Iberian Peninsula. It also includes a small exclave inside France called Llívia, as well as the Balearic Islands in the Mediterranean, the Canary Islands in the Atlantic Ocean 108 km (67 mi) off northwest Africa, and five places of sovereignty on and off the coast of North Africa: Ceuta, Melilla, Islas Chafarinas, Peñón de Alhucemas, and Peñón de Vélez de la Gomera.

<span class="mw-page-title-main">Subarctic climate</span> Climate characterised by long, usually very cold winters, and short, cool summers

The subarctic climate is a continental climate with long, cold winters, and short, warm to cool summers. It is found on large landmasses, often away from the moderating effects of an ocean, generally at latitudes from 50°N to 70°N, poleward of the humid continental climates. Subarctic or boreal climates are the source regions for the cold air that affects temperate latitudes to the south in winter. These climates represent Köppen climate classification Dfc, Dwc, Dsc, Dfd, Dwd and Dsd.

<span class="mw-page-title-main">Climate of the United Kingdom</span>

The United Kingdom straddles the higher mid-latitudes between 49° and 61°N on the western seaboard of Europe. Since the UK is always in or close to the path of the polar front jet stream, frequent changes in pressure and unsettled weather are typical. Many types of weather can be experienced in a single day.

<span class="mw-page-title-main">Rain shadow</span> Leeward side of a mountain range

A rain shadow is an area of significantly reduced rainfall behind a mountainous region, on the side facing away from prevailing winds, known as its leeward side.

<span class="mw-page-title-main">Mount Waialeale</span> Shield volcano and the second highest point on the island of Kauaʻi in the Hawaiian Islands

Mount Waiʻaleʻale is a shield volcano and the second highest point on the island of Kauaʻi in the Hawaiian Islands. Its name literally means "rippling water" or "overflowing water".

<span class="mw-page-title-main">Cherrapunji</span> Town in Meghalaya, India

Cherrapunji or Sohra is a sub-divisional town East Khasi Hills district in the Indian state of Meghalaya. It was the traditional capital of ka hima Sohra.

<span class="mw-page-title-main">Climate of Scotland</span>

The climate of Scotland is mostly temperate and oceanic, and tends to be very changeable, but rarely extreme. It is warmed by the Gulf Stream from the Atlantic, and given its northerly latitude it is much warmer than areas on similar latitudes, for example Kamchatka in Russia or Labrador in Canada, or Fort McMurray, Canada. Scots sometimes describe weather which is grey and gloomy using the Scots language word dreich.

<span class="mw-page-title-main">Cameroon line</span> Chain of volcanoes in the Gulf of Guinea

The Cameroon line is a 1,600 km (1,000 mi) long chain of volcanoes that includes islands in the Gulf of Guinea and mountains on the African mainland, from Mount Cameroon on the coast towards Lake Chad on the northeast. They form a natural border between eastern Nigeria and the West Region of Cameroon. The islands, which span the equator, have tropical climates and are home to many unique plant and bird species. The mainland mountain regions are much cooler than the surrounding lowlands, and also contain unique and ecologically important environments.

<span class="mw-page-title-main">Climate of Australia</span>

Australia's climate is governed mostly by its size and by the hot, sinking air of the subtropical high pressure belt. This moves north-west and north-east with the seasons. The climate is variable, with frequent droughts lasting several seasons, thought to be caused in part by the El Niño-Southern Oscillation. Australia has a wide variety of climates due to its large geographical size. The largest part of Australia is desert or semi-arid. Only the south-east and south-west corners have a temperate climate and moderately fertile soil. The northern part of the country has a tropical climate, varying between grasslands and desert. Australia holds many heat-related records: the continent has the hottest extended region year-round, the areas with the hottest summer climate, and the highest sunshine duration.

<span class="mw-page-title-main">Western High Plateau</span> Mountainous area in Cameroon

The Western High Plateau, Western Highlands or Bamenda Grassfields is a region of Cameroon characterised by high relief, cool temperatures, heavy rainfall and savanna vegetation. The region lies along the Cameroon line and consists of mountain ranges and volcanoes made of crystalline and igneous rock. The region borders the South Cameroon Plateau to the southeast, the Adamawa Plateau to the northeast and the Cameroon coastal plain to the south.

<span class="mw-page-title-main">Climate of Georgia (U.S. state)</span> Overview of the climate of the U.S. state of Georgia

The climate of Georgia is a humid subtropical climate, with most of the state having short, mild winters and long, hot summers. The Atlantic Ocean on the east coast of Georgia and the hill country in the north impact the state's climate. Also, the Chattahoochee River divides Georgia into separate climatic regions with the mountain region to the northwest being cooler than the rest of the state; the average temperatures for the mountain region in January and July are 39 °F (4 °C) and 78 °F (26 °C) respectively. Winter in Georgia is characterized by mild temperatures and little snowfall around the state, with the potential for snow and ice increasing in the northern parts of the state. Summer daytime temperatures in Georgia often exceed 95 °F (35 °C). The state experiences widespread precipitation. Tornadoes and tropical cyclones are common.

<span class="mw-page-title-main">Climate of North Carolina</span> Overview of the climate of the U.S. state of North Carolina

North Carolina's climate is varying, from the Atlantic coast in the east to the Appalachian Mountain range in the west. The mountains often act as a "shield", blocking low temperatures and storms from the Midwest from entering the Piedmont and Coastal Plain of North Carolina.

<span class="mw-page-title-main">Climate of Ireland</span>

The climate of Ireland is mild, humid and changeable with abundant rainfall and a lack of temperature extremes. Ireland's climate is defined as a temperate oceanic climate, or Cfb on the Köppen climate classification system, a classification it shares with most of northwest Europe. The island receives generally warm summers and cool winters.

The climate of Cameroon is very diverse. Cameroon is generally referred to as the Africa in miniature because it has the major climates and vegetation of the continent. The country is separated in two mains climatic zones: the equatorial climate in the south and the tropical climate in the northern part.

<span class="mw-page-title-main">Rain</span> Precipitation in the form of water droplets

Rain is water droplets that have condensed from atmospheric water vapor and then fall under gravity. Rain is a major component of the water cycle and is responsible for depositing most of the fresh water on the Earth. It provides water for hydroelectric power plants, crop irrigation, and suitable conditions for many types of ecosystems.

<span class="mw-page-title-main">Earth rainfall climatology</span> Study of rainfall

Earth rainfall climatology Is the study of rainfall, a sub-field of meteorology. Formally, a wider study includes water falling as ice crystals, i.e. hail, sleet, snow. The aim of rainfall climatology is to measure, understand and predict rain distribution across different regions of planet Earth, a factor of air pressure, humidity, topography, cloud type and raindrop size, via direct measurement and remote sensing data acquisition. Current technologies accurately predict rainfall 3–4 days in advance using numerical weather prediction. Geostationary orbiting satellites gather IR and visual wavelength data to measure realtime localised rainfall by estimating cloud albedo, water content, and the corresponding probability of rain.

<span class="mw-page-title-main">Geography of Washington (state)</span> Overview of the Geography of Washington

Washington is the northwesternmost state of the contiguous United States. It borders Idaho to the east, bounded mostly by the meridian running north from the confluence of the Snake River and Clearwater River, except for the southernmost section where the border follows the Snake River. Oregon is to the south, with the Columbia River forming the western part and the 46th parallel forming the eastern part of the Oregon–Washington border. During Washington's partition from Oregon, the original plan for the border followed the Columbia River east until the confluence with the Snake, and then would have followed the Snake River east; this was changed to keep Walla Walla's fertile farmland in Washington.

References

  1. Frankham, Richard; Ballou, Jonathan D.; Briscoe, David Anthony (2004). A primer of conservation genetics. Cambridge University Press. p. 180. ISBN   978-0-521-53827-5 . Retrieved 2011-11-12.
  2. "The World's Wettest Places". Thetravelalmanac.com. Retrieved 2011-11-12.
  3. Rowlett, Russ. "Lighthouses of Cameroon". The Lighthouse Directory. University of North Carolina at Chapel Hill . Retrieved 2011-11-12.
  4. "Picasa Web Albums - R. Burnstone - Cameroon". 2008-02-14. Archived from the original on 2012-07-13. Retrieved 2011-11-12.
  5. Česky. "Mount Cameroon Volcano, Africa (world) - facts & information / VolcanoDiscovery". Volcanodiscovery.com. Retrieved 2011-11-12.
  6. Harrison, Ian (June 20, 2008). "The Rainiest Places on Earth". blog.ratestogo.com. Archived from the original on October 31, 2011. Retrieved October 29, 2010.
  7. "Extreme precipitation events in Cameroon". ictp.it. The Abdus Salam International Centre for Theoretical Physics. Archived from the original on 2012-03-31.
  8. "Climate of the Mount Cameroon Region". Research Gate. Retrieved June 18, 2024.