What are the Climatic Floors of Ecuador?

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David Holt
What are the Climatic Floors of Ecuador?

The climatic floors of Ecuador are the different levels of variation of the climate of the region depending on its relief (altitude). Although it is generally said that the determining factor between one climatic floor and another is height, other elements such as air currents also play an important role..

In Ecuador there are 5 climatic floors: warm, temperate, cold, moor and glacial. These have different vegetation, fauna, climate and atmospheric conditions.

The main factor between climatic floors is temperature, which is directly related to altitude.

What are the climatic floors of Ecuador?

The five climatic floors of Ecuador are divided depending on the height at which they are.

Warm

Located between 0 and a thousand meters, it has a relatively pleasant temperature that averages 25 degrees Celsius.

The variation in temperature is practically zero, so it is often said that in this climatic floor there is only one season; the warm.

There is abundant rainfall and highly varied ecosystems, such as forests, savannas, jungles, and grasslands. The flora and fauna present great biodiversity and are very abundant.

Tempered

Between one thousand and two thousand meters are the areas with a temperate climate.

The variation of heat is more notable than in the warm floor, being able to differentiate clearly the winter - where the temperatures are of about 16 degrees centigrade - of the summer - where they rise up to 23-.

It is a floor that also has high levels of precipitation, however the rains are much more frequent in some areas than in others (although they share the same altitude), and are influenced by air currents..

Cold

It is between 2 thousand and 3 thousand meters.

Its average annual temperature is 12 degrees Celsius, which provides a comfortable environment, which is why many cities and urban settlements are located on this climatic floor, including Quito, the capital of Ecuador..

Like the temperate floor, the presence of precipitation has a certain dependence on air currents. The level of rain in the cold floor is lower than the warm and warm.

Paramo

From 3,000 to 4,000 meters there is the moorland, the fauna decreases considerably and the vegetation does so partially.

Despite the harsh climate and temperatures close to zero degrees, there are forests and bushes.

Glacial or perpetual snow

Above 4 thousand meters, temperatures drop below zero, there is no appreciable flora or fauna and rainfall occurs in the form of snow..

Name perpetual snow It is because the areas are permanently covered with snow and ice.

Factors that affect climatic floors

The most notable difference between the climatic floors of the same area is the temperature, since it decreases significantly as the altitude increases.. 

However, the variation in height can also increase or decrease the humidity, atmospheric pressure and amount of precipitation of a climatic floor..

In the case of Ecuador, in addition to the temperature, its proximity to the Andes mountain range and the air currents (such as the Humboldt) affect the climatic conditions of the different thermal floors..

References

  1. David Duañas (May 3, 2016). Climatic Floors of Ecuador. Retrieved on October 28, 2017, from Climatic Floors of Ecuador.
  2. Climate And Average Weather In Ecuador (s.f.). Retrieved on October 28, 2017, from World Weather and Climate.
  3. Peru Current (October 8, 2015). Retrieved on October 28, 2017, from Encyclopædia Britannica.
  4. Andean páramo (s.f.). Retrieved on October 28, 2017, from Wikipedia.
  5. 10 characteristics of the warm climate (s.f.). Retrieved on October 28, 2017, from Features.
  6. Polar Climates (s.f.). Retrieved on October 28, 2017, from Histórico Digital.
  7. Ecuador: weather November 85, 2007). Retrieved on October 28, 2017, from La Guía 2000.
  8. Temperate climate (s.f.). Retrieved on October 28, 2017, from Ecured.

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