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Chalpi | |
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Coordinates: 0°22′31.27″S78°4′39.58″W / 0.3753528°S 78.0776611°W | |
Country | Ecuador |
Province | Napo |
Canton | Quijos |
Elevation | 3,052 m (10,013 ft) |
Time zone | UTC-5 (Ecuador Time) |
Chalpi is a village in Quijos canton, Napo Province in Ecuador.
Chalpi has a Subtropical highland climate (Cfb) with cool weather year-round and moderately heavy rainfall.
Climate data for Chalpi | |||||||||||||
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Month | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | Year |
Average high °C (°F) | 16.4 (61.5) | 16.2 (61.2) | 15.8 (60.4) | 16.0 (60.8) | 15.7 (60.3) | 14.7 (58.5) | 14.4 (57.9) | 14.8 (58.6) | 15.5 (59.9) | 16.5 (61.7) | 17.0 (62.6) | 16.6 (61.9) | 15.8 (60.4) |
Daily mean °C (°F) | 11.1 (52.0) | 11.1 (52.0) | 11.1 (52.0) | 11.3 (52.3) | 11.1 (52.0) | 10.4 (50.7) | 10.1 (50.2) | 10.3 (50.5) | 10.7 (51.3) | 11.2 (52.2) | 11.6 (52.9) | 11.2 (52.2) | 10.9 (51.7) |
Average low °C (°F) | 5.9 (42.6) | 6.1 (43.0) | 6.5 (43.7) | 6.7 (44.1) | 6.6 (43.9) | 6.1 (43.0) | 5.9 (42.6) | 5.8 (42.4) | 5.9 (42.6) | 6.0 (42.8) | 6.2 (43.2) | 5.9 (42.6) | 6.1 (43.0) |
Average precipitation mm (inches) | 103 (4.1) | 86 (3.4) | 106 (4.2) | 119 (4.7) | 131 (5.2) | 123 (4.8) | 126 (5.0) | 107 (4.2) | 107 (4.2) | 104 (4.1) | 94 (3.7) | 81 (3.2) | 1,287 (50.8) |
Source: Climate-Data.org [1] |
Climate is the long-term weather pattern in an area, typically averaged over 30 years. More rigorously, it is the mean and variability of meteorological variables over a time spanning from months to millions of years. Some of the meteorological variables that are commonly measured are temperature, humidity, atmospheric pressure, wind, and precipitation. In a broader sense, climate is the state of the components of the climate system, including the atmosphere, the hydrosphere, the cryosphere, the lithosphere and the biosphere and the interactions between them. The climate of a location is affected by its latitude/longitude, terrain, altitude, and nearby water bodies and their currents.
The Intergovernmental Panel on Climate Change (IPCC) is an intergovernmental body of the United Nations responsible for advancing knowledge on human-induced climate change. It was established in 1988 by the World Meteorological Organization (WMO) and the United Nations Environment Programme (UNEP), and later endorsed by United Nations General Assembly. Headquartered in Geneva, Switzerland, it is composed of 195 member states.
The Kyoto Protocol was an international treaty which extended the 1992 United Nations Framework Convention on Climate Change (UNFCCC) that commits state parties to reduce greenhouse gas emissions, based on the scientific consensus that (part one) global warming is occurring and (part two) that human-made CO2 emissions are driving it. The Kyoto Protocol was adopted in Kyoto, Japan, on 11 December 1997 and entered into force on 16 February 2005. There were 192 parties (Canada withdrew from the protocol, effective December 2012) to the Protocol in 2020.
The United Nations Framework Convention on Climate Change (UNFCCC) established an international environmental treaty to combat "dangerous human interference with the climate system", in part by stabilizing greenhouse gas concentrations in the atmosphere. It was signed by 154 states at the United Nations Conference on Environment and Development (UNCED), informally known as the Earth Summit, held in Rio de Janeiro from 3 to 14 June 1992. It established a Secretariat headquartered in Bonn and entered into force on 21 March 1994. The treaty called for ongoing scientific research and regular meetings, negotiations, and future policy agreements designed to allow ecosystems to adapt naturally to climate change, to ensure that food production is not threatened and to enable economic development to proceed in a sustainable manner.
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In geography, the temperate climates of Earth occur in the middle latitudes, which span between the tropics and the polar regions of Earth. These zones generally have wider temperature ranges throughout the year and more distinct seasonal changes compared to tropical climates, where such variations are often small and usually only have precipitation changes.
The desert climate or arid climate, is a climate in which there is a severe excess of evaporation over precipitation. The typically bald, rocky, or sandy surfaces in desert climates are dry and hold little moisture, quickly evaporating the already little rainfall they receive. Covering 14.2% of earth's land area, hot deserts are the second most common type of climate on earth after the polar climate.
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A humid continental climate is a climatic region defined by Russo-German climatologist Wladimir Köppen in 1900, typified by four distinct seasons and large seasonal temperature differences, with warm to hot summers and freezing cold winters. Precipitation is usually distributed throughout the year but often do have dry seasons. The definition of this climate regarding temperature is as follows: the mean temperature of the coldest month must be below 0 °C (32.0 °F) or −3 °C (26.6 °F) depending on the isotherm, and there must be at least four months whose mean temperatures are at or above 10 °C (50 °F). In addition, the location in question must not be semi-arid or arid. The cooler Dfb, Dwb, and Dsb subtypes are also known as hemiboreal climates.
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