altitude

1. The height of a thing above a reference level, especially above sea level or above the earth's surface. See synonyms at elevation.
2. A high location or area.
3. Astronomy. The angular distance of a celestial object above the horizon.
4. Mathematics. The perpendicular distance from the base of a geometric figure to the opposite vertex, parallel side, or parallel surface.
5. High position or rank.

[Middle English, from Latin altitūdō, from altus, high.]

There is no precise definition of high altitude. However, many people feel lightheaded and have other symptoms if they ascend from near sea level to 3000 metres (about 10 000 feet). Some individuals are affected at as low as 2000 metres. Nearly 140 million people live at altitudes above 2500 metres (about 8000 feet). Substantial numbers live permanently at altitudes as high as 4500 metres in the Peruvian Andes, and caretakers of a mine in Chile have lived at nearly 6000 metres. The highest point on Earth is the summit of Mt. Everest (8848 metres), and well-acclimatized climbers can just reach that altitude without using supplementary oxygen.

The two regions of the world with the largest high-altitude populations are the South American Andes and the Tibetan plateau. It is estimated that between 10 and 17 million people live at over 2500 metres in the Andes, and that over 50 000 people in Peru reside above 4000 metres. Lhasa, in Tibet, altitude 3658 metres, has over 130 000 inhabitants. Other parts of the world with substantial high-altitude populations include Central and North America, Europe, Russia, Africa, and Indonesia.

It is useful to divide people at high altitude into two groups; those who live there permanently (‘highlanders’) and those who have moved up temporarily from sea level (‘lowlanders’). Lowlanders who go to high altitude undergo a process known as acclimatization, which greatly assists them in tolerating the high altitude. Some permanent residents who have been at high altitude for generations have probably undergone true Darwinian adaptation. Many features of acclimatization and adaptation are similar, but there are some differences.

Fig. 1 Altitude and oxygen pressures. Modified, with author's approval, from J. B. West Respiratory physiology — the essentials. 6th edition, Lippincott Williams and Wilkins, Philadelphia, 2000.

Altitude and oxygen

High altitude provides physiological and medical challenges because the amount of oxygen in the air is reduced. As we go higher, the barometric pressure falls, for the same reason as, when we are submerged deeper in water, the pressure rises. Indeed, Torricelli, who invented the mercury barometer in the mid-seventeenth century, stated, ‘We live submerged at the bottom of an ocean of the element air, which by unquestioned experiments is known to have weight.’ For example, if we go to an altitude of about 5800 metres, the pressure falls to half the normal sea level value of 760 mm Hg (1013 millibars or hectopascals). At the summit of Mt. Everest the pressure is about one-third of the sea level value. Since oxygen accounts for one-fifth of the volume of the air, and this fraction does not alter with altitude, the pressure of oxygen decreases proportionally with the total barometric pressure. A decrease in this ‘partial pressure’ of oxygen in the lungs results in a decrease in the amount of oxygen in the blood — the state of oxygen shortage, or hypoxia. This hypoxia is responsible for almost all the physiological changes and the potential medical problems that occur at high altitude.

The relationship between barometric pressure and altitude is not the same over the whole surface of the globe. Because of the warming of the atmosphere by the sun near the Equator, the column of air is higher there, and therefore the barometric pressure at any given altitude is higher than at the poles. These differences are important to the mountain climber. For example, it can be shown that if Mt. Everest were at the latitude of Mt. McKinley (Denali) in Alaska, which is 60° N, the summit would in effect be over 950 metres (3000 feet) higher because the barometric pressure at high altitude at latitudes far from the Equator is so much lower. This would make it impossible to climb the mountain without supplementary oxygen. On the other hand, the use of the International Civil Aviation Organization (ICAO) Standard Atmosphere (often used to calibrate altimeters) considerably underestimates the barometric pressure on the summit of Everest: the severity of hypoxia was therefore overestimated in some predictions based on this method in the past.

Acclimatization

The role of acclimatization in enabling lowlanders to tolerate high altitude is critical; indeed it is one of the classical examples of how the human body can adapt to hostile conditions. A normal person who is acutely exposed to the barometric pressure of the summit of Mt. Everest in a low-pressure chamber will lose consciousness within 2 or 3 minutes, but with the advantages of acclimatization, many climbers have now reached the summit without supplementary oxygen.

The most important feature of acclimatization to high altitude is an increase in the rate and depth of breathing. The product of the volume of each breath multiplied by the frequency of breathing is known as the total ventilation. The increase in ventilation is brought about by stimulation of chemoreceptors by the low oxygen pressure in the arterial blood. A chemoreceptor is a specialized tissue which responds to its environment by sending nerve impulses to the brain. In order for a climber to reach the Everest summit, he must increase his ventilation some 5-fold. Anecdotal evidence of this comes from tape recordings of climbers on the summit; they are so short of breath that they need to breathe after every two or three words! The reason why the increase in ventilation is so important is that it raises the pressure of oxygen in the alveoli in the depths of the lung, where the exchange between the air and blood takes place. At the same time, the increase in ventilation greatly reduces the pressure of carbon dioxide in the lungs and in the blood.

The extent to which people increase their breathing when they go to high altitude depends on their genetic make-up: some increase it much more than others. There is some evidence that climbers who have a poor ventilatory response to hypoxia tolerate very high altitudes badly. A test for this can be administered at sea level by giving people a low-oxygen mixture to breathe.

Interestingly, many people who are born at high altitude have a relatively low ventilatory response to hypoxia. This seems to be paradoxical, although it may protect them from periodic breathing during sleep (see below). It may be that these permanent residents have other adaptations at the tissue level which are not yet understood.

Another feature of acclimatization is an increase in the concentration of red cells in the blood. For example, a permanent resident at 4600 metres in the Peruvian Andes typically has a 30% increase in red cell concentration. This polycythaemia increases the oxygen carrying capacity of the blood. However, the value of polycythaemia in the acclimatization process is not as clear as it was once thought to be. Severe polycythaemia increases the viscosity of the blood and probably leads to problems with unloading oxygen from the blood to the tissues. Some permanent residents of the Andes can actually do more physical work when the concentration of red cells in their blood is reduced by bloodletting.

The mechanism responsible for polycythaemia is the release of the hormone erythropoietin from the kidney as a result of the shortage of oxygen there. The erythropoietin then stimulates the production of red blood cells by the bone marrow. The evolutionary pressure for the development of this mechanism probably occurred at sea level, promoting survival after injury, because blood loss also causes inadequacy of oxygen supply. It may be that its value as an adaptation to high altitude has been overemphasized.

The cardiac output increases with acute hypoxia, compensating for the shortage of oxygen in the blood by increasing the rate of blood supply, but in acclimatized subjects it returns to the sea level value. Other features of acclimatization include an increase in the concentration of capillaries in peripheral tissues, and increases in the amount of oxidative enzymes within cells. It is likely that some of the acclimatization processes at the cellular level have not yet been discovered.

Many features of the adaptation of permanent residents to high altitude are similar to those of acclimatization. Interestingly, there is some evidence that Tibetans have progressed further in the adaptation process than Andeans, consistent with the much longer period that they have spent at high altitude. Features that suggest better adaptation include less polycythaemia, greater ventilation, lower pressures in the pulmonary circulation, and an apparent lower incidence of ‘chronic mountain sickness’ (see below). However, this is an active area of research and there is some controversy.

Mount Everest

One of the great sagas of this century has been the ascent of Mt. Everest without supplementary oxygen. In 1920 the mountaineer-physiologist Alexander Kellas predicted that it could be done if the technical difficulties were not too great. During the 1924 British expedition to Everest, E. F. Norton climbed to within 300 metres of the summit without supplementary oxygen, but in the 1930s several physiological studies suggested that the summit could not be reached. It was not until 1978, 54 years after Norton, that the last 300 metres were conquered by Messner and Habeler.

The critical factors on the summit are the barometric pressure, the extent of the increase in the climber's ventilation, and his maximal oxygen uptake. The first measurements of these were obtained by the American Medical Research Expedition to Everest in 1981. In 1985 a simulated climb in a low-pressure chamber, Operation Everest II, greatly clarified the physiological adaptations at extreme altitudes, particularly in the pulmonary circulation and skeletal muscle. For example, the resistance of the pulmonary circulation was greatly increased at very high altitudes, because hypoxia constricted the blood vessels. Also, muscle biopsies showed an increase in the concentration of capillaries because the muscle fibres became thinner.

Altitude sickness

Various forms of altitude sickness are recognized. Newcomers to high altitude frequently complain of headache, fatigue, dizziness, palpitations, nausea, loss of appetite, and insomnia. This is known as acute mountain sickness, and usually resolves after 2 or 3 days at medium altitudes. It is probably caused by the combination of the low oxygen and the alkalosis in the blood resulting from the reduced pressure of carbon dioxide. Administration of the drug acetazolamide reduces the incidence of acute mountain sickness.

A more severe illness is high-altitude pulmonary oedema, in which the capillaries in the lung are damaged and leak high-protein fluid into the alveolar spaces. The damage is due to high pressures in the pulmonary circulation, which develop in response to the hypoxia. This potentially fatal condition is best treated by taking the patient down to a lower altitude as rapidly as possible, though oxygen is given if this is available. An even more serious problem is high-altitude cerebral oedema due to leakage of fluid into the brain tissues. Again, descent is by far the best treatment. Long-term residents at high altitude sometimes develop an ill-defined syndrome characterized by fatigue, reduced ability to exercise, very low levels of oxygen in the blood, and marked polycythaemia. This is called chronic mountain sickness, and again descent is the best treatment if this is practicable.

Newcomers to high altitude often complain that the most distressing period is during the night when they try to sleep. Periodic breathing frequently occurs. This is characterized by a gradual waxing and then waning of breathing movements, and often there is a period of no breathing at all (apnea) which may last for 10 sec or more. Sometimes people wake up at the end of the apneic period feeling smothered. Treatment with acetazolamide reduces the incidence and severity of periodic breathing. Permanent residents of high altitude who have a reduced ventilatory response to hypoxia develop less periodic breathing.

Factors other than hypoxia

All of the physiological and medical problems of going to high altitude described above have their root in the low partial pressure of oxygen in the air. This is an inevitable consequence of going to high altitude unless, of course, supplementary oxygen is breathed. However there are other potentially hostile factors at high altitude. One is cold. The air temperature falls at the rate of about 1 °C for every 150 metres of altitude. The effects of cold can of course be mitigated by warm clothing and shelter, but if there is a high wind the resulting chill factor makes it impossible to climb at great altitudes.

Another potential problem results from the low absolute humidity of the air because of the low temperatures. Climbers frequently become dehydrated because they lose a great deal of water vapour as a result of their high ventilation, and it is difficult to obtain water by melting snow. Solar radiation is increased at high altitude because of reduced absorption by the thinner atmosphere, and reflection of the sun from snow. Ionizing radiation, for example by cosmic rays, is also increased because of the thinner atmosphere.

Working at high altitude

Recently there has been a large increase in commercial and scientific facilities, such as mines and telescopes, at very high altitudes. Much of this development has taken place in the Andes, particularly in north Chile. As an example, the Collahuasi copper mine at an altitude of 4500 metres was being greatly expanded in the late 1990s. The workers live at sea level and are taken by bus up to the mine in a few hours, where they spend the next seven days working. They are then taken down to their families at sea level for seven days, and the cycle continues indefinitely. This cycling raises many physiological and medical problems which are poorly understood as yet. Another example is a new radiotelescope being planned for an altitude of 5000 metres in north Chile. The workers will live at an altitude of about 2400 metres and commute up to the telescope each day.

An interesting innovation is the addition of oxygen to the air conditioning in these facilities, in dormitories, offices, conference rooms, laboratories, and even in the cabins of large trucks and mechanical shovels. Every 1% of enrichment (for example increasing the oxygen concentration from 21% to 22%) is equivalent to reducing the altitude by 300 metres. Five per cent oxygen enrichment in a mine at 4500 metres could therefore reduce the equivalent altitude to 3000 metres, which is much more easily tolerated. Oxygen enrichment has become feasible because large amounts of oxygen can easily be produced from air by oxygen concentrators, and also because liquid oxygen is relatively inexpensive. The potential value of this proactive approach to dealing with the hypoxia of high altitude is still being clarified.

— John B. West

Bibliography

• Ward, M. P., Milledge, J. S., and West, J. B. (2000). High altitude medicine and physiology, (3rd edn). Arnold, London.
• West, J. B. (1985). Everest — the testing place. McGraw-Hill, New York

See also flying; hypoxia; oxygen.

As altitude increases, air temperature and pressure decrease and there is less oxygen available for aerobic activities. This lack of oxygen can severely limit the physical performance of endurance athletes and climbers, particularly those accustomed to living at low altitudes. The thin air, however, offers less resistance to sprinters and jumpers, so it is generally easier to perform these activities at high altitudes than at sea level.

High altitudes are potentially dangerous environments. Anyone who ascends too quickly above 2100 metres can become sick. Individuals differ in their susceptibility to altitude or mountain sickness, but nearly everyone suffers above a height of 4900 metres. Twenty five per cent of visitors to the Colorado skiing areas, just 3000 metres above sea level, suffer some form of altitude sickness. The risk appears to be less if you sleep at a lower altitude than the one at which you are active; the mountaineer's advice ‘play high, sleep low’ appears to be sound.

Altitude sickness is caused by lack of oxygen and is characterized by shortness of breath, feelings of lassitude, muscular weakness, headaches, rapid pulse, loss of appetite, nausea, and sometimes fainting. The symptoms become more severe the higher a person ascends and the faster the ascent is made, but they usually quickly disappear when the sufferer returns to lower altitudes and rests.

It can be fatal to continue climbing when suffering from altitude sickness. Each year several people die in high mountain regions such as the Himalayas. The situation is likely to worsen as more people take to the mountains on organized expedition treks. Altitude sickness is best avoided by ascending slowly, drinking plenty of fluids (non-alcoholic!), and giving your body the opportunity to acclimatize to low oxygen levels.

Altitude acclimatization consists of a number of reversible physiological adaptations. These enable the body to cope with low oxygen levels. In the early stages of acclimatization, breathing and heart rate increase. Major long-term adaptations include the production of more red blood cells, an increase in the haemoglobin content of the blood, and a greater blood supply to muscles. All these adaptations help to improve the ability of the blood to carry oxygen to respiring tissues. Biochemical changes also help the muscles to utilize oxygen more efficiently. Acclimatization to medium altitudes (1829 m above sea level) takes about two weeks, but acclimatization to high altitudes (more than 3048 m above sea level) may take much longer.

Many elite athletes train at medium altitudes to benefit from the effects of altitude acclimatization and to enhance performance in endurance events. Most exercise scientists believe that the training is of significant benefit only to those who intend competing at high altitudes, and that it is of little benefit to sea-level competitors. To be effective, altitude training must take place at least 1500 metres above sea level and for a period of not less than three weeks, with the first week consisting of light exercise only. It is, however, risky to train at altitudes for very long periods because it may lead to loss of muscle and body weight. It takes three to six weeks at sea level to lose all the effects of altitude training and acclimatization.

noun

The distance of something from a given level: elevation, height. See high/low.

Definition: height
Antonyms: depth

n

Definition: height in the sky
Antonyms: depth

Pertaining to any location on earth with reference to a fixed surface point, which is usually sea level. The higher the altitude, the lower the oxygen concentration and the greater the ultraviolet radiation, both of which can cause health problems.

The vertical distance above sea level. Medium altitudes are between 1829 and 3048 m above sea level; high altitudes are higher than 3048 m above sea level. As altitude increases, the barometric pressure decreases and oxygen partial pressures become lower, reducing maximal oxygen uptake. In addition, temperature drops at a rate of 1°C for every 150 m. Maximal oxygen uptake decreases as altitude increases above 1600 m; consequently, both medium and high altitude can adversely affect performance in endurance activities, particularly in those who normally live at sea level. Short-term anaerobic performance capacity is not adversely affected by medium altitude. On the contrary, the rarified atmosphere can be beneficial to sprinters, throwers, and jumpers. See also altitude acclimatization, altitude training.

(DOD, NATO) The vertical distance of a level, a point or an object considered as a point, measured from mean sea level. See also density altitude; drop altitude; elevation; minimum safe altitude; pressure altitude; transition altitude; true altitude.

Tutor's tip: If a plane flies at a high "altitude," it is at a certain elevation above the earth or sea level. If you don't like flying, it could harm your "attitude" (feeling or idea about something).

For other uses, see Altitude (disambiguation).

Altitude is defined based on the context in which it is used (aviation, geometry, geographical survey, sport, and more). 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.

Vertical distance measurements in the "down" direction are commonly referred to as depth.

Contents 1 Altitude in aviation 2 Altitude in sport 3 Altitude regions 4 References 5 External links 6 See also

Altitude in aviation

Vertical Distance Comparison

In aviation, the term altitude can have several meanings, and is always qualified by either explicitly adding a modifier (e.g. "true altitude"), or implicitly through the context of the communication. Parties exchanging altitude information must be clear which definition is being used.^[1]

Aviation altitude is measured using either Mean Sea Level (MSL) or local ground level (Above Ground Level, or AGL) as the reference datum.

With the exception of a few countries whose aviation authorities use metres (e.g. Russia), altitudes are stated in feet.

Pressure altitude divided by 100 feet is referred to as the flight level, and is used above the transition altitude (18,000 feet in the US, but may be as low as 3,000 feet in other jurisdictions); so when the altimeter reads 18,000 ft on the standard pressure setting the aircraft is said to be at "Flight level 180". When flying at a Flight Level, the altimeter is always set to standard pressure (29.92 / 1013.25).

On the flight deck, the definitive instrument for measuring altitude is the pressure altimeter, which is an aneroid barometer with a front face indicating distance (feet or metres) instead of atmospheric pressure.

There are several types of aviation altitude:

• Indicated altitude is the reading on the altimeter when the altimeter is set to the local barometric pressure at Mean Sea Level.
• Absolute altitude is the height of the aircraft above the terrain over which it is flying. Also referred to feet/metres Above Ground Level (AGL).
• True altitude is the elevation above mean sea level. In UK aviation radiotelephony usage, the vertical distance of a level, a point or an object considered as a point, measured from mean sea level; this is referred to over the radio as altitude.(see QNH)^[2]
• Height is the elevation above a ground reference point, commonly the terrain elevation. In UK aviation radiotelephony usage, the vertical distance of a level, a point or an object considered as a point, measured from a specified datum; this is referred to over the radio as height, where the specified datum is the airfield elevation (see QFE)^[2]
• Pressure altitude is the elevation above a standard datum air-pressure plane (typically, 1013.25 millibars or 29.92" Hg and 15°C). Pressure altitude and indicated altitude are the same when the altimeter is set to 29.92" Hg or 1013.25 millibars.
• Density altitude is the altitude corrected for non-ISA International Standard Atmosphere atmospheric conditions. Aircraft performance depends on density altitude, which is affected by barometric pressure, humidity and temperature. On a very hot day, density altitude at an airport (especially one at a high elevation) may be so high as to preclude takeoff, particularly for helicopters or a heavily loaded aircraft.

These types of altitude can be explained more simply as various ways of measuring the altitude:

• Indicated altitude -- what the altimeter says
• Absolute altitude -- altitude in terms of the distance above the ground directly below it
• True altitude -- altitude in terms of elevation above sea level
• Height -- altitude in terms of the distance above a certain point
• Pressure altitude -- altitude in terms of the air pressure
• Density altitude -- altitude in terms of the density of the air

Altitude in sport

Atmospheric pressure decreases as altitude increases, and as the pressure decreases less oxygen is available for sportsmen to utilise. These are the basis for two contradictory effects of high altitude on exercise and sport. For explosive events (sprints up to 400 metres, long jump, triple jump) the reduction in atmospheric pressure means there is less resistance from the atmosphere and the athlete's performance will generally be better at high altitude. For endurance events (races of 5000 metres or more) the predominant effect is the reduction in oxygen which generally reduces the athlete's performance at high altitude.

Living at high altitude causes the body to physiologically adapt to the reduction in available oxygen (a process known as acclimatization) so that an advantage in oxygen take-up is evidenced when the athlete returns to a lower altitude.^[3] These changes are the basis of altitude training which forms an integral part of the training of athletes in a number of endurance sports including track and field, distance running, triathlon, cycling and swimming.

Sports organisations also acknowledge the effects of altitude on performance. The International Association of Athletic Federations (IAAF), for example, have ruled that performances achieved at an altitude greater than 1000 metres will not be approved for record purposes.

Altitude regions

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.

Mountain medicine recognizes three altitude regions:^[4]

• High altitude = 1500 m – 3500 m (5000 – 11,500 ft)
• Very High altitude = 3500 m – 5500 m (11,500 – 18,000 ft)
• Extreme altitude = 5500 m – above

Travel to high altitudes can lead to medical problems, from the mild symptoms of acute mountain sickness to the potentially fatal high altitude pulmonary oedema (HAPE) and high altitude cerebral oedema (HACE). These conditions are caused by the profound hypoxia associated with travel to high altitudes.^[5]

The Earth's atmosphere is divided into several altitude regions:^[6]

• Troposphere — surface to 8000 m / 5 miles at poles – 18,000 m / 11 miles at equator, ending at the Tropopause.
• Stratosphere — Troposphere to 50 km /31 miles
• Mesosphere — Stratosphere to 85 km /53 miles
• Thermosphere — Mesosphere to 675 km / 420 miles
• Exosphere — Thermosphere to 10,000 km /6200 miles

References

1. ^ Air Navigation. Department of the Air Force. 1 December 1989. AFM 51-40. 
2. ^ ^{a b} Radiotelephony Manual. UK Civil Aviation Authority. 1 January 1995. CAP413. ISBN 0860396010. 
3. ^ Muza, SR; Fulco, CS; Cymerman, A (2004). "Altitude Acclimatization Guide.". US Army Research Inst. of Environmental Medicine Thermal and Mountain Medicine Division Technical Report (USARIEM-TN-04-05). http://archive.rubicon-foundation.org/7616. Retrieved 2009-03-05. 
4. ^ "Non-Physician Altitude Tutorial". International Society for Mountain Medicine. http://www.ismmed.org/np_altitude_tutorial.htm. Retrieved 22 December 2005. 
5. ^ Cymerman, A; Rock, PB. Medical Problems in High Mountain Environments. A Handbook for Medical Officers. USARIEM-TN94-2. US Army Research Inst. of Environmental Medicine Thermal and Mountain Medicine Division Technical Report. http://archive.rubicon-foundation.org/7976. Retrieved 2009-03-05. 
6. ^ "Layers of the Atmosphere". JetStream, the National Weather Service Online Weather School. National Weather Service. http://www.srh.noaa.gov/srh/jetstream/atmos/layers.htm. Retrieved 22 December 2005. 

External links

• "Altitude pressure calculator". Apex (altitude physiology expeditions). http://www.altitude.org/calculators/airpressure.htm. Retrieved 2006-08-08. 
• "The Race to the Stratosphere". U.S. Centennial of Flight Commission. http://www.centennialofflight.gov/essay/Lighter_than_air/race_to_strato/LTA11.htm. Retrieved 25 January 2006. 
• Downloadable ETOPO2 Raw Data Database (2 minute grid)
• Downloadable ETOPO5 Raw Data Database (5 minute grid)
• Calculate true altitude with these JavaScript applications

See also

• Altitude sickness
• Death zone
• Flight altitude record
• High altitude pulmonary edema
• High altitude cerebral edema
• High altitude wind power

This entry is from Wikipedia, the leading user-contributed encyclopedia. It may not have been reviewed by professional editors (see full disclaimer)

Dansk (Danish)
n. - højde

idioms:

• altitude sickness    højdesyge

Nederlands (Dutch)
hoogte, verhevenheid, hevigheid (van gevoel etc.)

Français (French)
n. - altitude, hauteur

idioms:

• altitude sickness    (avoir) le mal d'altitude

Deutsch (German)
n. - Höhe

idioms:

• altitude sickness    Höhenkrankheit

Ελληνική (Greek)
n. - ύψος, υψόμετρο, (αστρον.) ύψος, έξαρμα

idioms:

• altitude sickness    ζαλάδα λόγω υψομέτρου

Italiano (Italian)
altitudine, altezza

idioms:

• altitude sickness    mal d'altitudine

Português (Portuguese)
n. - altitude (f), altura (f) (Astr.) (Geom.), eminência (f)

idioms:

• altitude sickness    mal (m) das alturas (Med.)

Русский (Russian)
высота

idioms:

• altitude sickness    высотная болезнь

Español (Spanish)
n. - altura, altitud

idioms:

• altitude sickness    mal de alturas, apunamiento

Svenska (Swedish)
n. - höjd, topp

中文（简体）(Chinese (Simplified))
高, 高度, 高处, 高地, 海拔, 顶垂线, 高线

idioms:

• altitude sickness    高空病

中文（繁體）(Chinese (Traditional))
n. - 高, 高度, 高處, 高地, 海拔, 頂垂線, 高線

idioms:

• altitude sickness    高空病

한국어 (Korean)
n. - 높이, 해발

日本語 (Japanese)
n. - 高さ, 高度, 海抜, 標高, 高所, 高い地位

idioms:

• altitude sickness    高山病, 高所病

العربيه (Arabic)
‏(الاسم) الارتفاع‏

עברית (Hebrew)
n. - ‮גובה, רום‬

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