relative humidity oor Thai
relative humidity
en
The ratio of the actual amount of water vapor (absolute humidity) present in the air to the saturation point at the same temperature, usually expressed as a percentage.
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Relative humidity: 5% to 90% noncondensing
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Relative humidity: 0% to 90% noncondensing
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Climate: Mostly arid, with low rainfall and low relative humidity
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Relative humidity: 5% to 95% noncondensing
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Rel. Humidity
โหมด OpenGLKDE40.1 KDE40.1
The experiments suggested that "N. fusca" grows best when relative humidity is in the range of 65 to 90%.
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By the time the air reaches the farthest point in your lungs, it has a relative humidity of almost 100 percent.
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In the winter relative humidity can reach 95 percent without raining, and the well-adapted Limeños, residents of Lima, bundle up against the damp, penetrating cold.
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Relative humidity is normally expressed as a percentage; a higher percentage means that the air–water mixture is more humid. At 100% relative humidity, the air is saturated and is at its dew point.
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Due to the night-time temperature drop, relative air humidity increases significantly, rising from 65–75% to over 95%.
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This and other basic principles indicate that warming associated with increased concentrations of the other greenhouse gases also will increase the concentration of water vapor (assuming that the relative humidity remains approximately constant; modeling and observational studies find that this is indeed so). Because water vapor is a greenhouse gas, this results in further warming and so is a "positive feedback" that amplifies the original warming.
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Potentials below 3000 volts are not typically detectable by humans. Maximal potential commonly achieved on human body range between 1 and 10 kV, though in optimal conditions as high as 20–25 kV can be reached. Low relative humidity increases the charge buildup; walking 20 feet (6 m) on vinyl floor at 15% relative humidity causes buildup of voltage up to 12 kV, while at 80% humidity the voltage is only 1.5 kV.
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Maximal potential commonly achieved on human body range between 1 and 10 kV, though in optimal conditions as high as 20–25 kV can be reached. Low relative humidity increases the charge buildup; walking 20 feet (6 m) on vinyl floor at 15% relative humidity causes buildup of voltage up to 12 kV, while at 80% humidity the voltage is only 1.5 kV. As little as 0.2 millijoules may present an ignition hazard; such low spark energy is often below the threshold of human visual and auditory perception.
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The energy efficiency ratio (EER) of a particular cooling device is the ratio of "output" cooling energy (in BTU/hr) to "input" electrical energy (in Watts) at a given operating point. EER is generally calculated using a 95 °F outside temp and an inside (actually return air) temp of 80 °F and 50% relative humidity. The EER is related to the coefficient of performance (COP) commonly used in thermodynamics, with the primary difference being that the COP of a cooling device is unit-less, because the numerator and denominator are expressed in the same units.
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In the upper limit of its range, night-time temperatures may approach freezing and day-time maxima rarely exceed 25 °C. Due to the night-time temperature drop, relative air humidity increases significantly, rising from 65–75% to over 95%. Vegetation at this height is very stunted and slow-growing due to the extreme environmental conditions that prevail.
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Summers are hot and humid, but winters are relatively cold with occasional snowfall. Kyoto's rain season begins around the middle of June and lasts until the end of July, yielding to a hot and sunny latter half of the summer.
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Plants are often subjected to fierce winds and driving rain, as well as exposure to intense direct sunlight. The relatively open vegetation of the upper montane forest also experiences greater fluctuations in temperature and humidity compared with lower altitudes. These changes are largely governed by the extent of cloud cover.
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The majority of the country lies within the Tropical savanna climate zone, as the coastal areas in the South and West receive noticeably more and steady rain before and during the wet season. These areas constitute the easternmost fringes of the south-west monsoon, determined to be inside the Tropical monsoon climate. Countrywide there are two seasons of relatively equal length, defined by varying precipitation as temperatures and humidity are generally high and steady throughout the entire year.
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18 sinne gevind in 5 ms. Hulle kom uit baie bronne en word nie nagegaan nie.