Lac De Charpal (lake)
Region: Languedoc-Roussillon, France
Lac De Charpal is a lake in the region of Languedoc-Roussillon, the country of France with an average elevation of 1,331 meter above sea level. The location is sparsely populated with 6 people per km2 . The nearest town larger than 50,000 inhabitants takes about 3:40 hour by local transportation.
The child mortality is 4 per 1,000 births.
Lac De Charpal can have low impact (v or less) earthquakes (on average one every 50 years), with occurances at <5 Richter. When an earthquake occurs, it may be felt indoors by many people, outdoors by a few people during the day. At night, some people may be awakened. There is a very low occurence of periods with extreme drought. Flooding risk is extremely high.
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Weather
July is warmest with an average temperature of 19.4 °C at noon. February is coldest with an average temperature of -4.7 °C at night. Lac De Charpal has temperate cold and warm seasons, like winters and summers. The temperatures at night are cooler than during daytime.
Winters have some periods of frost, with the coldest month most often being December. July is on average the month with most sunshine. Rainfall and other precipitation has no distinct peak month.
More weather patterns, current and forecast......
Time
Today's sunrise occurs around 6:00 AM and the sunset is around 9:34 PM. Usually a clear night sky is not polluted by light from unnatural sources, it makes looking at stars easy at night.
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| Name |
Lac de Charpal |
| Type |
Lake |
| Lat./Long. |
44.617 / 3.567 |
| Country |
 France |
| Elevation |
1,331 meter |
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Nature
Lac De Charpal has a humid (> 0.65 p/pet) climate. The land area is not cultivated, most of the natural vegetation is still intact. The landscape is mostly covered with closed to open mixed broadleaved and needleleaved forest. The climate is classified as a subartic (severe winter, no dry season with a cool temperate moist forest biozone . The soil in the area is high in cambisols (cm), moderately developed soils with lower horizons having color or structure changes from the parent material which permit the identification of a cambic b horizon.
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