Alpine climate

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White Mountain, an alpine environment at 4,300 metres (14,000 ft) in California, USA. White Mountain CA.JPG
White Mountain, an alpine environment at 4,300 metres (14,000 ft) in California, USA.

Alpine climate is the average weather (climate) for the regions above the tree line. This climate is also referred to as a mountain climate or highland climate.

Weather state of the atmosphere

Weather is the state of the atmosphere, describing for example the degree to which it is hot or cold, wet or dry, calm or stormy, clear or cloudy. Most weather phenomena occur in the lowest level of the atmosphere, the troposphere, just below the stratosphere. Weather refers to day-to-day temperature and precipitation activity, whereas climate is the term for the averaging of atmospheric conditions over longer periods of time. When used without qualification, "weather" is generally understood to mean the weather of Earth.

Climate Statistics of weather conditions in a given region over long periods

Climate is the statistics of weather over long periods of time. It is measured by assessing the patterns of variation in temperature, humidity, atmospheric pressure, wind, precipitation, atmospheric particle count and other meteorological variables in a given region over long periods of time. Climate differs from weather, in that weather only describes the short-term conditions of these variables in a given region.

Tree line edge of the habitat at which trees are capable of growing

The tree line is the edge of the habitat at which trees are capable of growing. It is found at high elevations and high latitudes. Beyond the tree line, trees cannot tolerate the environmental conditions. The tree line is sometimes distinguished from a lower timberline or forest line, which is the line below which trees form a forest with a closed canopy.

Contents

Definition

There are multiple definitions of alpine climate.

One simple definition is the climate which causes trees to fail to grow due to cold. According to the Holdridge life zone system, alpine climate occurs when the mean biotemperature of a location is between 1.5 and 3 °C (34.7 and 37.4 °F), which prevents tree growth. Biotemperature is defined as the mean temperature, except all temperatures below 0 °C (32 °F) are treated as 0 °C (32 °F), because plants are dormant below freezing. [1]

In the Köppen climate classification, the alpine climate is part of "Group E", along with the polar climate, where no month has a mean temperature higher than 10 °C (50 °F). [2]

Köppen climate classification widely used climate classification system

The Köppen climate classification is one of the most widely used climate classification systems. It was first published by the Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system.

Polar climate Rosa Melano es hermana de Elver Galarga

The polar climate regions are characterized by a lack of warm summers. Every month in a polar climate has an average temperature of less than 10 °C (50 °F). Regions with polar climate cover more than 20% of the Earth. Most of these regions are far from the equator, and in this case, winter days are extremely short and summer days are extremely long. A polar climate consists of cool summers and very cold winters, which results in treeless tundra, glaciers, or a permanent or semi-permanent layer of ice.

Temperature physical property of matter that quantitatively expresses the common notions of hot and cold

Temperature is a physical quantity expressing hot and cold. It is measured with a thermometer calibrated in one or more temperature scales. The most commonly used scales are the Celsius scale, Fahrenheit scale, and Kelvin scale. The kelvin is the unit of temperature in the International System of Units (SI), in which temperature is one of the seven fundamental base quantities. The Kelvin scale is widely used in science and technology.

Cause

The temperature profile of the atmosphere is a result of an interaction between radiation and convection. Sunlight in the visible spectrum hits the ground and heats it. The ground then heats the air at the surface. If radiation were the only way to transfer heat from the ground to space, the greenhouse effect of gases in the atmosphere would keep the ground at roughly 333 K (60 °C; 140 °F), and the temperature would decay exponentially with height. [3]

Radiation waves or particles propagating through space or through a medium, carrying energy

In physics, radiation is the emission or transmission of energy in the form of waves or particles through space or through a material medium. This includes:

Convection movement of groups of molecules within fluids such as liquids or gases, and within rheids; takes place through advection, diffusion or both

Convection is the heat transfer due to the bulk movement of molecules within fluids such as gases and liquids, including molten rock (rheid). Convection includes sub-mechanisms of advection, and diffusion.

Visible spectrum portion of the electromagnetic spectrum that is visible to the human eye

The visible spectrum is the portion of the electromagnetic spectrum that is visible to the human eye. Electromagnetic radiation in this range of wavelengths is called visible light or simply light. A typical human eye will respond to wavelengths from about 380 to 740 nanometers. In terms of frequency, this corresponds to a band in the vicinity of 430–770 THz.

However, when air is hot, it tends to expand, which lowers its density. Thus, hot air tends to rise and transfer heat upward. This is the process of convection. Convection comes to equilibrium when a parcel of air at a given altitude has the same density as its surroundings. Air is a poor conductor of heat, so a parcel of air will rise and fall without exchanging heat. This is known as an adiabatic process, which has a characteristic pressure-temperature curve. As the pressure gets lower, the temperature decreases. The rate of decrease of temperature with elevation is known as the adiabatic lapse rate, which is approximately 9.8 °C per kilometer (or 5.4 °F per 1000 feet) of altitude. [3]

Adiabatic process thermodynamic process

An adiabatic process occurs without transfer of heat or mass of substances between a thermodynamic system and its surroundings. In an adiabatic process, energy is transferred to the surroundings only as work. The adiabatic process provides a rigorous conceptual basis for the theory used to expound the first law of thermodynamics, and as such it is a key concept in thermodynamics.

Note that the presence of water in the atmosphere complicates the process of convection. Water vapor contains latent heat of vaporization. As air rises and cools, it eventually becomes saturated and cannot hold its quantity of water vapor. The water vapor condenses (forming clouds), and releases heat, which changes the lapse rate from the dry adiabatic lapse rate to the moist adiabatic lapse rate (5.5 °C per kilometre or 3 °F per 1000 feet). [4] The actual lapse rate, called the environmental lapse rate, is not constant (it can fluctuate throughout the day or seasonally and also regionally), but a normal lapse rate is 5.5 °C per 1,000 m (3.57 °F per 1,000 ft). [5] [6] Therefore, moving up 100 metres (330 ft) on a mountain is roughly equivalent to moving 80 kilometres (45 miles or 0.75° of latitude) towards the pole. [7] This relationship is only approximate, however, since local factors, such as proximity to oceans, can drastically modify the climate. [8] As the altitude increases, the main form of precipitation becomes snow and the winds increase. The temperature continues to drop until the tropopause, at 11,000 metres (36,000 ft), where it does not decrease further. However, this is higher than the highest summit.

Dew point

The dew point is the temperature to which air must be cooled to become saturated with water vapour. When further cooled, the airborne water vapor will condense to form liquid water (dew). When air cools to its dew point through contact with a surface that is colder than the air, water will condense on the surface. When the temperature is below the freezing point of water, the dew point is called the frost point, as frost is formed rather than dew. The measurement of the dew point is related to humidity. A higher dew point means there will be more moisture in the air.

Cloud visible mass of liquid droplets or frozen crystals suspended in the atmosphere

In meteorology, a cloud is an aerosol consisting of a visible mass of minute liquid droplets, frozen crystals, or other particles suspended in the atmosphere of a planetary body. Water or various other chemicals may compose the droplets and crystals. On Earth, clouds are formed as a result of saturation of the air when it is cooled to its dew point, or when it gains sufficient moisture from an adjacent source to raise the dew point to the ambient temperature. They are seen in the Earth's homosphere. Nephology is the science of clouds, which is undertaken in the cloud physics branch of meteorology.

Latitude The angle between zenith at a point and the plane of the equator

In geography, latitude is a geographic coordinate that specifies the north–south position of a point on the Earth's surface. Latitude is an angle which ranges from 0° at the Equator to 90° at the poles. Lines of constant latitude, or parallels, run east–west as circles parallel to the equator. Latitude is used together with longitude to specify the precise location of features on the surface of the Earth. On its own, the term latitude should be taken to be the geodetic latitude as defined below. Briefly, geodetic latitude at a point is the angle formed by the vector perpendicular to the ellipsoidal surface from that point, and the equatorial plane. Also defined are six auxiliary latitudes which are used in special applications.

Distribution

Although this climate classification only covers a small portion of the Earth's surface, alpine climates are widely distributed. For example, The Sierra Nevada, the Cascade Mountains, the Rocky Mountains, the Appalachian Mountains, and the summit of Mauna Loa in the United States, the Alps, the Trans-Mexican volcanic belt, the Snowy Mountains in Australia, the Pyrenees, Cantabrian Mountains and Sierra Nevada in Spain, the Andes, the Himalayas, the Tibetan Plateau, Gansu, and Qinghai in China, the Eastern Highlands of Africa, high elevations in the Atlas Mountains and the central parts of Borneo and New Guinea.

The lowest altitude of alpine climate varies dramatically by latitude. If alpine climate is defined by the tree line, then it occurs as low as 650 metres (2,130 ft) at 68°N in Sweden, [9] while on Mount Kilimanjaro in Africa, the alpine climate and the tree line are met at 3,950 metres (12,960 ft). [9]

Monthly variability

The variability of the alpine climate throughout the year depends on the latitude of the location. For tropical oceanic locations, such as the summit of Mauna Loa, elev. 13,679 ft (4,169 m), the temperature is roughly constant throughout the year:

Climate data for Mauna Loa slope observatory (1961–1990)
MonthJanFebMarAprMayJunJulAugSepOctNovDecYear
Record high °F (°C)67
(19)
85
(29)
65
(18)
67
(19)
68
(20)
71
(22)
70
(21)
68
(20)
67
(19)
66
(19)
65
(18)
67
(19)
85
(29)
Average high °F (°C)49.8
(9.9)
49.6
(9.8)
50.2
(10.1)
51.8
(11.0)
53.9
(12.2)
57.2
(14.0)
56.4
(13.6)
56.3
(13.5)
55.8
(13.2)
54.7
(12.6)
52.6
(11.4)
50.6
(10.3)
53.2
(11.8)
Average low °F (°C)33.3
(0.7)
32.9
(0.5)
33.2
(0.7)
34.6
(1.4)
36.6
(2.6)
39.4
(4.1)
38.8
(3.8)
38.9
(3.8)
38.5
(3.6)
37.8
(3.2)
36.2
(2.3)
34.3
(1.3)
36.2
(2.3)
Record low °F (°C)19
(−7)
18
(−8)
20
(−7)
24
(−4)
27
(−3)
28
(−2)
26
(−3)
28
(−2)
29
(−2)
27
(−3)
25
(−4)
22
(−6)
18
(−8)
Average precipitation inches (mm)2.3
(58)
1.5
(38)
1.7
(43)
1.3
(33)
1.0
(25)
0.5
(13)
1.1
(28)
1.5
(38)
1.3
(33)
1.1
(28)
1.7
(43)
2.0
(51)
17
(431)
Average snowfall inches (cm)0.0
(0.0)
1.0
(2.5)
0.3
(0.76)
1.3
(3.3)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
1.0
(2.5)
3.6
(9.06)
Average precipitation days (≥ 0.01 inch)45654345555455
Source: NOAA [10]

For mid-latitude locations, such as Mount Washington the temperature varies, but never gets very warm:

Climate data for Mount Washington, elev. 6,267 ft (1,910.2 m) near the summit
MonthJanFebMarAprMayJunJulAugSepOctNovDecYear
Record high °F (°C)48
(9)
43
(6)
54
(12)
60
(16)
66
(19)
72
(22)
71
(22)
72
(22)
69
(21)
62
(17)
52
(11)
47
(8)
72
(22)
Average high °F (°C)13.6
(−10.2)
14.7
(−9.6)
20.7
(−6.3)
30.4
(−0.9)
41.3
(5.2)
50.4
(10.2)
54.1
(12.3)
53.3
(11.8)
47.1
(8.4)
36.4
(2.4)
28.1
(−2.2)
18.4
(−7.6)
34.0
(1.1)
Daily mean °F (°C)4.8
(−15.1)
6.2
(−14.3)
12.9
(−10.6)
23.9
(−4.5)
35.6
(2.0)
45.0
(7.2)
49.1
(9.5)
48.2
(9.0)
41.6
(5.3)
30.2
(−1.0)
20.7
(−6.3)
10.1
(−12.2)
27.4
(−2.6)
Average low °F (°C)−4.1
(−20.1)
−2.4
(−19.1)
5.0
(−15.0)
17.4
(−8.1)
29.8
(−1.2)
39.5
(4.2)
44.0
(6.7)
43.0
(6.1)
36.1
(2.3)
24.0
(−4.4)
13.3
(−10.4)
1.7
(−16.8)
20.6
(−6.3)
Record low °F (°C)−47
(−44)
−46
(−43)
−38
(−39)
−20
(−29)
−2
(−19)
8
(−13)
24
(−4)
20
(−7)
9
(−13)
−5
(−21)
−20
(−29)
−46
(−43)
−47
(−44)
Average precipitation inches (mm)6.44
(164)
6.77
(172)
7.67
(195)
7.44
(189)
8.18
(208)
8.40
(213)
8.77
(223)
8.32
(211)
8.03
(204)
9.27
(235)
9.85
(250)
7.73
(196)
96.87
(2,460)
Average snowfall inches (cm)44.0
(112)
40.1
(102)
45.1
(115)
35.6
(90)
12.2
(31)
1.0
(2.5)
0.0
(0.0)
0.1
(0.25)
2.2
(5.6)
17.6
(45)
37.8
(96)
45.5
(116)
281.2
(714)
Average precipitation days (≥ 0.01 in)19.717.919.017.417.416.816.515.213.916.819.120.7210.4
Average snowy days (≥ 0.1 in)19.317.316.613.16.40.90.10.21.79.114.619.2118.5
Mean monthly sunshine hours 92.0106.9127.6143.2171.3151.3145.0130.5127.2127.182.483.11,487.6
Percent possible sunshine 32363435373331303437293033
Source #1: NOAA (normals 1981–2010, sun 1961–1990) [11] [12] [13]
Source #2: extremes 1933–present [14] [15]

See also

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Mountain A large landform that rises fairly steeply above the surrounding land over a limited area

A mountain is a large landform that rises above the surrounding land in a limited area, usually in the form of a peak. A mountain is generally steeper than a hill. Mountains are formed through tectonic forces or volcanism. These forces can locally raise the surface of the earth. Mountains erode slowly through the action of rivers, weather conditions, and glaciers. A few mountains are isolated summits, but most occur in huge mountain ranges.

Troposphere The lowest layer of the atmosphere

The troposphere is the lowest layer of Earth's atmosphere, and is also where nearly all weather conditions take place. It contains approximately 75% of the atmosphere's mass and 99% of the total mass of water vapor and aerosols. The average height of the troposphere is 18 km in the tropics, 17 km in the middle latitudes, and 6 km in the polar regions in winter. The total average height of the troposphere is 13 km.

Altitude or height is defined based on the context in which it is used. As a general definition, altitude is a distance measurement, usually in the vertical or "up" direction, between a reference datum and a point or object. The reference datum also often varies according to the context. Although the term altitude is commonly used to mean the height above sea level of a location, in geography the term elevation is often preferred for this usage.

Water vapor gaseous phase of water; unlike other forms of water, water vapor is invisible

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Alpine tundra biome

Alpine tundra is a type of natural region or biome that does not contain trees because it is at high elevation. As the latitude of a location approaches the poles, the threshold elevation for alpine tundra gets lower until it reaches sea level, and alpine tundra merges with polar tundra.

The lapse rate is the rate at which an atmospheric variable, normally temperature in Earth's atmosphere, changes with altitude. Lapse rate arises from the word lapse, in the sense of a gradual change. It corresponds to the vertical component of the spatial gradient of temperature. Although this concept is most often applied to the Earth's troposphere, it can be extended to any gravitationally supported parcel of gas.

Equivalent potential temperature, commonly referred to as theta-e , is a quantity that is conserved during changes to an air parcel's pressure, even if water vapor condenses during that pressure change. It is therefore more conserved than the ordinary potential temperature, which remains constant only for unsaturated vertical motions.

International Standard Atmosphere Atmospheric model

The International Standard Atmosphere (ISA) is a static atmospheric model of how the pressure, temperature, density, and viscosity of the Earth's atmosphere change over a wide range of altitudes or elevations. It has been established to provide a common reference for temperature and pressure and consists of tables of values at various altitudes, plus some formulas by which those values were derived. The International Organization for Standardization (ISO) publishes the ISA as an international standard, ISO 2533:1975. Other standards organizations, such as the International Civil Aviation Organization (ICAO) and the United States Government, publish extensions or subsets of the same atmospheric model under their own standards-making authority.

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Wet-bulb temperature temperature read by a thermometer covered in water-soaked cloth

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Convective instability

In meteorology, convective instability or stability of an air mass refers to its ability to resist vertical motion. A stable atmosphere makes vertical movement difficult, and small vertical disturbances dampen out and disappear. In an unstable atmosphere, vertical air movements tend to become larger, resulting in turbulent airflow and convective activity. Instability can lead to significant turbulence, extensive vertical clouds, and severe weather such as thunderstorms.

Level of free convection

The level of free convection (LFC) is the altitude in the atmosphere where the temperature of the environment decreases faster than the moist adiabatic lapse rate of a saturated air parcel at the same level.

Lifted condensation level

The lifted condensation level or lifting condensation level (LCL) is formally defined as the height at which the relative humidity (RH) of an air parcel will reach 100% with respect to liquid water when it is cooled by dry adiabatic lifting. The RH of air increases when it is cooled, since the amount of water vapor in the air remains constant, while the saturation vapor pressure decreases almost exponentially with decreasing temperature. If the air parcel is lifting further beyond the LCL, water vapor in the air parcel will begin condensing, forming cloud droplets. The LCL is a good approximation of the height of the cloud base which will be observed on days when air is lifted mechanically from the surface to the cloud base.

Atmospheric thermodynamics is the study of heat-to-work transformations that take place in the earth's atmosphere and manifest as weather or climate. Atmospheric thermodynamics use the laws of classical thermodynamics, to describe and explain such phenomena as the properties of moist air, the formation of clouds, atmospheric convection, boundary layer meteorology, and vertical instabilities in the atmosphere. Atmospheric thermodynamic diagrams are used as tools in the forecasting of storm development. Atmospheric thermodynamics forms a basis for cloud microphysics and convection parameterizations used in numerical weather models and is used in many climate considerations, including convective-equilibrium climate models.

The convective condensation level (CCL) represents the height where an air parcel becomes saturated when heated from below and lifted adiabatically due to buoyancy.

Atmospheric instability

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Montane ecosystems ecosystems found in mountains

Montane ecosystems refers to any ecosystem found in mountains. These ecosystems are strongly affected by climate, which gets colder as elevation increases. They are stratified according to elevation. Dense forests are common at moderate elevations. However, as the elevation increases, the climate becomes harsher, and the plant community transitions to grasslands or tundra.

Glossary of meteorology Wikimedia list article

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References

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