Dew point - wikipedia Dew point This article is about the meteorological dew point. For the petroleum term, see Hydrocarbon dew point. Humidity and hygrometry Specific concepts Absolute / Specific / Relative Dew point ( depression ) Psychrometrics General concepts Air Concentration Density Dew Evaporation Humidity buffering ( Atm. ) Pressure Liquid water Avogadro 's law Nucleation Thermodynamic equilibrium Measures and Instruments Heat index Sat. vap. density Mixing ratio Water activity H. indicator card Hygrometer Dry / Wet - bulb temperature The dew point is the temperature to which air must be cooled to become saturated with water vapor. 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. Contents 1 Humidity 2 Relationship to human comfort 3 Measurement 4 Extreme values 5 Calculating the dew point 5.1 Simple approximation 6 Frost point 7 See also 8 References 9 External links Humidity Given that all the other factors influencing humidity remain constant, at ground level the relative humidity rises as the temperature falls. This is because less vapor is needed to saturate the air so, vapor condenses as the temperature falls. Dew point temperature is never greater than the air temperature because relative humidity can not exceed 100 %. In technical terms, the dew point is the temperature at which the water vapor in a sample of air at constant barometric pressure condenses into liquid water at the same rate at which it evaporates. At temperatures below the dew point, the rate of condensation will be greater than that of evaporation, forming more liquid water. The condensed water is called dew when it forms on a solid surface, or frost if it freezes. The condensed water is called either fog or a cloud, depending on its altitude, when it forms in the air. A high relative humidity implies that the dew point is closer to the current air temperature. A relative humidity of 100 % indicates the dew point is equal to the current temperature and that the air is maximally saturated with water. When the moisture content remains constant and temperature increases, relative humidity decreases. General aviation pilots use dew point data to calculate the likelihood of carburetor icing and fog, and to estimate the height of a cumuliform cloud base. This graph shows the maximum percentage, by mass, of water vapor that air at sea - level pressure across a range of temperatures can contain. For a lower ambient pressure, a curve has to be drawn above the current curve. A higher ambient pressure yields a curve under the current curve. At a given temperature but independent of barometric pressure, the dew point is a consequence of the absolute humidity, the mass of water per unit volume of air. If both the temperature and pressure rise, however, the dew point will increase and the relative humidity will decrease accordingly. Reducing the absolute humidity without changing other variables will bring the dew point back down to its initial value. In the same way, increasing the absolute humidity after a temperature drop brings the dew point back down to its initial level. If the temperature rises in conditions of constant pressure, then the dew point will remain constant but the relative humidity will drop. For this reason, a constant relative humidity with different temperatures implies that when it is hotter, a higher fraction of the air is present as water vapor compared to when it is cooler. At a given barometric pressure but independent of temperature, the dew point indicates the mole fraction of water vapor in the air, or, put differently, determines the specific humidity of the air. If the pressure rises without changing this mole fraction, the dew point will rise accordingly. Reducing the mole fraction, i.e., making the air less humid, would bring the dew point back down to its initial value. In the same way, increasing the mole fraction after a pressure drop brings the relative humidity back up to its initial level. Considering New York ( 33 ft or 10 m elevation ) and Denver ( 5,280 ft or 1,610 m elevation ), for example, this means that if the dew point and temperature in both cities are the same, then the mass of water vapor per cubic meter of air will be the same, but the mole fraction of water vapor in the air will be greater in Denver. Relationship to human comfort This section needs additional citations for verification. Please help improve this article by adding citations to reliable sources. Unsourced material may be challenged and removed. ( October 2016 ) When the air temperature is high, the human body uses the evaporation of sweat to cool down, with the cooling effect directly related to how fast the perspiration evaporates. The rate at which perspiration can evaporate depends on how much moisture is in the air and how much moisture the air can hold. If the air is already saturated with moisture, perspiration will not evaporate. The body 's thermoregulation will produce perspiration in an effort to keep the body at its normal temperature even when the rate it is producing sweat exceeds the evaporation rate, so one can become coated with sweat on humid days even without generating additional body heat ( such as by exercising ). As the air surrounding one 's body is warmed by body heat, it will rise and be replaced with other air. If air is moved away from one 's body with a natural breeze or a fan, sweat will evaporate faster, making perspiration more effective at cooling the body. The more unevaporated perspiration, the greater the discomfort. A wet bulb thermometer also uses evaporative cooling, so it provides a good measure for use in evaluating comfort level. Discomfort also exists when the dew point is low ( below around − 30 ° C or − 22 ° F ). The drier air can cause skin to crack and become irritated more easily. It will also dry out the airways. The US Occupational Safety and Health Administration recommends indoor air be maintained at 20 -- 24.5 ° C ( 68 -- 76 ° F ) with a 20 -- 60 % relative humidity, equivalent to a dew point of − 4.5 to 15.5 ° C ( 24 to 60 ° F ). Lower dew points, less than 10 ° C or 50 ° F, correlate with lower ambient temperatures and the body requires less cooling. A lower dew point can go along with a high temperature only at extremely low relative humidity, allowing for relatively effective cooling. People inhabiting tropical and subtropical climates acclimatize somewhat to higher dew points. Thus, a resident of Darwin or Miami, for example, might have a higher threshold for discomfort than a resident of a temperate climate like London or Chicago. Those accustomed to temperate climates often begin to feel uncomfortable when the dew point reaches between 15 and 20 ° C ( 59 -- 68 ° F ), while others might find dew points below 18 ° C ( 64 ° F ) comfortable. Most inhabitants of these areas will consider dew points above 21 ° C or 70 ° F oppressive and tropical - like. Dew point Human perception Relative humidity at 32 ° C ( 90 ° F ) Over 26 ° C Over 80 ° F Severely high, even deadly for asthma related illnesses 73 % and higher 24 -- 26 ° C 75 -- 80 ° F Extremely uncomfortable, oppressive 62 -- 72 % 21 -- 24 ° C 70 -- 74 ° F Very humid, quite uncomfortable 52 -- 61 % 18 -- 21 ° C 65 -- 69 ° F Somewhat uncomfortable for most people at upper edge 44 -- 51 % 16 -- 18 ° C 60 -- 64 ° F OK for most, but all perceive the humidity at upper edge 37 -- 43 % 13 -- 16 ° C 55 -- 59 ° F Comfortable 31 -- 36 % 10 -- 12 ° C 50 -- 54 ° F Very comfortable 26 -- 30 % Under 10 ° C Under 50 ° F A bit dry for some 25 % and lower Measurement Devices called hygrometers are used to measure dew point over a wide range of temperatures. These devices consist of a polished metal mirror which is cooled as air is passed over it. The temperature at which dew forms is, by definition, the dew point. Manual devices of this sort can be used to calibrate other types of humidity sensors, and automatic sensors may be used in a control loop with a humidifier or dehumidifier to control the dew point of the air in a building or in a smaller space for a manufacturing process. Extreme values A dew point of 33 ° C ( 91 ° F ) was observed at 14 : 00 EDT on July 12, 1987, in Melbourne, Florida. A dew point of 32 ° C ( 90 ° F ) has been observed in the United States on at least two other occasions : Appleton, Wisconsin, at 17 : 00 CDT on July 13, 1995, and New Orleans Naval Air Station at 17 : 00 CDT on July 30, 1987. A dew point of 35 ° C ( 95 ° F ) was observed at Dhahran, Saudi Arabia, at 15 : 00 AST on July 8, 2003, which caused the heat index to reach 81 ° C ( 178 ° F ), the highest value recorded. Calculating the dew point Graph of the dependence of the dew point upon air temperature for several levels of relative humidity. See also : Psychrometric chart A well - known approximation used to calculate the dew point, T, given just the actual ( `` dry bulb '' ) air temperature, T ( in degrees Celsius ) and relative humidity ( in percent ), RH, is the Magnus formula : γ ( T, R H ) = ln ⁡ ( R H 100 ) + b T c + T ; T d p = c γ ( T, R H ) b − γ ( T, R H ) ; ( displaystyle ( \begin ( aligned ) gamma ( T, mathrm ( RH ) ) & = ln left ( ( \frac ( mathrm ( RH ) ) ( 100 ) ) \right ) + ( \frac ( bT ) ( c + T ) ) ; ( 8pt ) T_ ( mathrm ( dp ) ) & = ( \frac ( c gamma ( T, mathrm ( RH ) ) ) ( b - gamma ( T, mathrm ( RH ) ) ) ) ; end ( aligned ) ) ) The more complete formulation and origin of this approximation involves the interrelated saturated water vapor pressure ( in units of millibars, also called hectopascals ) at T, P ( T ), and the actual vapor pressure ( also in units of millibars ), P ( T ), which can be either found with RH or approximated with the barometric pressure ( in millibars ), BP, and `` wet - bulb '' temperature, T is ( unless declared otherwise, all temperatures are expressed in degrees Celsius ) : P s ( T ) = 100 R H P a ( T ) = a e b T c + T ; P a ( T ) = R H 100 P s ( T ) = a e γ ( T, R H ) ≈ P s ( T w ) − B P m b 0.00066 ( 1 + 0.00115 T w ) ( T − T w ) ; T d p = c ln ⁡ P a ( T ) a b − ln ⁡ P a ( T ) a ; ( displaystyle ( \begin ( aligned ) P_ ( mathrm ( s ) ) ( T ) & = ( \frac ( 100 ) ( mathrm ( RH ) ) ) P_ ( mathrm ( a ) ) ( T ) = ae ^ ( \frac ( bT ) ( c + T ) ) ; ( 8pt ) P_ ( mathrm ( a ) ) ( T ) & = ( \frac ( mathrm ( RH ) ) ( 100 ) ) P_ ( mathrm ( s ) ) ( T ) = ae ^ ( gamma ( T, mathrm ( RH ) ) ) & approx P_ ( mathrm ( s ) ) ( T_ ( mathrm ( w ) ) ) - BP_ ( mathrm ( mb ) ) 0.00066 left ( 1 + 0.00115 T_ ( mathrm ( w ) ) \right ) left ( T - T_ ( mathrm ( w ) ) \right ) ; ( 8pt ) T_ ( mathrm ( dp ) ) & = ( \frac ( c ln ( \frac ( P_ ( mathrm ( a ) ) ( T ) ) ( a ) ) ) ( b - ln ( \frac ( P_ ( mathrm ( a ) ) ( T ) ) ( a ) ) ) ) ; end ( aligned ) ) ) For greater accuracy, P ( T ) ( and therefore γ ( T, RH ) ) can be enhanced, using part of the Bögel modification, also known as the Arden Buck equation, which adds a fourth constant d : P s, m ( T ) = a e ( b − T d ) ( T c + T ) ; γ m ( T, R H ) = ln ⁡ ( R H 100 e ( b − T d ) ( T c + T ) ) ; T d p = c γ m ( T, R H ) b − γ m ( T, R H ) ; ( displaystyle ( \begin ( aligned ) P_ ( mathrm ( s, m ) ) ( T ) & = ae ^ ( left ( b - ( \frac ( T ) ( d ) ) \right ) left ( ( \frac ( T ) ( c + T ) ) \right ) ) ; ( 8pt ) gamma _ ( mathrm ( m ) ) ( T, mathrm ( RH ) ) & = ln left ( ( \frac ( mathrm ( RH ) ) ( 100 ) ) e ^ ( left ( b - ( \frac ( T ) ( d ) ) \right ) left ( ( \frac ( T ) ( c + T ) ) \right ) ) \right ) ; ( 8pt ) T_ ( dp ) & = ( \frac ( c gamma _ ( m ) ( T, mathrm ( RH ) ) ) ( b - gamma _ ( m ) ( T, mathrm ( RH ) ) ) ) ; end ( aligned ) ) ) where a = 6.1121 mb, b = 18.678, c = 257.14 ° C, d = 234.5 ° C. There are several different constant sets in use. The ones used in NOAA 's presentation are taken from a 1980 paper by David Bolton in the Monthly Weather Review : a = 6.112 mb, b = 17.67, c = 243.5 ° C. These valuations provide a maximum error of 0.1 %, for − 30 ° C ≤ T ≤ 35 ° C and 1 % < RH < 100 %. Also noteworthy is the Sonntag1990, a = 6.112 mb, b = 17.62, c = 243.12 ° C ; for − 45 ° C ≤ T ≤ 60 ° C ( error ± 0.35 ° C ). Another common set of values originates from the 1974 Psychrometry and Psychrometric Charts, as presented by Paroscientific, a = 6.105 mb, b = 17.27, c = 237.7 ° C ; for 0 ° C ≤ T ≤ 60 ° C ( error ± 0.4 ° C ). Also, in the Journal of Applied Meteorology and Climatology, Arden Buck presents several different valuation sets, with different minimum accuracies for different temperature ranges. Two particular sets provide a range of − 40 ° C to + 50 ° C between the two, with even greater minimum accuracy than all of the other, above sets ( maximum error at extremes of temperature range ) : a = 6.1121 mb, b = 17.368, c = 238.88 ° C ; for 0 ° C ≤ T ≤ 50 ° C ( error ≤ 0.05 % ). a = 6.1121 mb, b = 17.966, c = 247.15 ° C ; for − 40 ° C ≤ T ≤ 0 ° C ( error ≤ 0.06 % ). Simple approximation There is also a very simple approximation that allows conversion between the dew point, temperature, and relative humidity. This approach is accurate to within about ± 1 ° C as long as the relative humidity is above 50 % : T d p ≈ T − 100 − R H 5 ; R H ≈ 100 − 5 ( T − T d p ) ; ( displaystyle ( \begin ( aligned ) T_ ( mathrm ( dp ) ) & approx T - ( \frac ( 100 - mathrm ( RH ) ) ( 5 ) ) ; ( 5pt ) mathrm ( RH ) & approx 100 - 5 ( T - T_ ( mathrm ( dp ) ) ) ; end ( aligned ) ) ) This can be expressed as a simple rule of thumb : For every 1 ° C difference in the dew point and dry bulb temperatures, the relative humidity decreases by 5 %, starting with RH = 100 % when the dew point equals the dry bulb temperature. The derivation of this approach, a discussion of its accuracy, comparisons to other approximations, and more information on the history and applications of the dew point are given in the Bulletin of the American Meteorological Society. For temperatures in degrees Fahrenheit, these approximations work out to T d p, ∘ F ≈ T ∘ F − 9 25 ( 100 − R H ) ; R H ≈ 100 − 25 9 ( T ∘ F − T d p, ∘ F ) ; ( displaystyle ( \begin ( aligned ) T_ ( mathrm ( dp, ^ ( circ ) F ) ) & approx T_ ( mathrm ( ( ) ^ ( circ ) F ) ) - ( \tfrac ( 9 ) ( 25 ) ) left ( 100 - mathrm ( RH ) \right ) ; ( 5pt ) mathrm ( RH ) & approx 100 - ( \tfrac ( 25 ) ( 9 ) ) left ( T_ ( mathrm ( ( ) ^ ( circ ) F ) ) - T_ ( mathrm ( dp, ^ ( circ ) F ) ) \right ) ; end ( aligned ) ) ) For example, a relative humidity of 100 % means dew point is the same as air temp. For 90 % RH, dew point is 3 ° F lower than air temperature. For every 10 percent lower, dew point drops 3 ° F. Frost point The frost point is similar to the dew point, in that it is the temperature to which a given parcel of humid air must be cooled, at constant barometric pressure, for water vapor to be deposited on a surface as ice without going through the liquid phase. ( Compare with sublimation. ) The frost point for a given parcel of air is always higher than the dew point, as the stronger bonding between water molecules on the surface of ice requires higher temperature to break. See also Bubble point Carburetor heat Hydrocarbon dew point Psychrometrics Thermodynamic diagrams References Jump up ^ Glossary - NOAA 's National Weather Service ^ Jump up to : John M. Wallace ; Peter V. Hobbs ( 24 March 2006 ). Atmospheric Science : An Introductory Survey. Academic Press. pp. 83 --. ISBN 978 - 0 - 08 - 049953 - 6. Jump up ^ Glossary - NOAA 's National Weather Service Jump up ^ Observed Dew Point Temperature : indicates the amount of moisture in the air Jump up ^ Dew Point Definition of dew point by Merriam - Webster ^ Jump up to : Horstmeyer, Steve ( 2006 - 08 - 15 ). `` Relative Humidity... Relative to What ? The Dew Point Temperature... a better approach ''. Steve Horstmeyer, Meteorologist, WKRC TV, Cincinnati, Ohio, USA. Retrieved 2009 - 08 - 20. Jump up ^ `` Denver Facts Guide -- Today ''. The City and County of Denver. Archived from the original on February 3, 2007. Retrieved March 19, 2007. Jump up ^ Relative Humidity and Dewpoint Temperature from Temperature and Wet - Bulb Temperature Jump up ^ Bolton, David ( July 1980 ). `` The Computation of Equivalent Potential Temperature '' ( PDF ). Monthly Weather Review. 108 ( 7 ) : 1046 -- 1053. Bibcode : 1980MWRv... 108.1046 B. doi : 10.1175 / 1520 - 0493 ( 1980 ) 108 < 1046 : TCOEPT > 2.0.CO ; 2. Jump up ^ SHTxx Application Note Dew - point Calculation Jump up ^ `` MET4 and MET4A Calculation of Dew Point ''. Archived from the original on May 26, 2012. Retrieved 7 October 2014. Jump up ^ Buck, Arden L. ( December 1981 ). `` New Equations for Computing Vapor Pressure and Enhancement Factor '' ( PDF ). Journal of Applied Meteorology. 20 ( 12 ) : 1527 -- 1532. Bibcode : 1981JApMe... 20.1527 B. doi : 10.1175 / 1520 - 0450 ( 1981 ) 020 < 1527 : NEFCVP > 2.0.CO ; 2. Jump up ^ Lawrence, Mark G. ( February 2005 ). `` The Relationship between Relative Humidity and the Dewpoint Temperature in Moist Air : A Simple Conversion and Applications ''. Bulletin of the American Meteorological Society. 86 ( 2 ) : 225 -- 233. Bibcode : 2005BAMS... 86... 225L. doi : 10.1175 / BAMS - 86 - 2 - 225. Jump up ^ Haby, Jeff. `` Frost point and dew point ''. Retrieved September 30, 2011. External links Often Needed Answers about Temp, Humidity & Dew Point from the sci. geo. meteorology Meteorological data and variables General Adiabatic processes Advection Buoyancy Lapse rate Lightning Surface solar radiation Surface weather analysis Visibility Vorticity Wind Wind shear Condensation Cloud Cloud condensation nuclei ( CCN ) Fog Convective condensation level ( CCL ) Lifted condensation level ( LCL ) Precipitation Water vapor Convection Convective available potential energy ( CAPE ) Convective inhibition ( CIN ) Convective instability Convective momentum transport Convective temperature ( T ) Equilibrium level ( EL ) Free convective layer ( FCL ) Helicity K Index Level of free convection ( LFC ) Lifted index ( LI ) Maximum parcel level ( MPL ) Bulk Richardson number ( BRN ) Temperature Dew point ( T ) Dew point depression Dry - bulb temperature Equivalent temperature ( T ) Forest fire weather index Haines Index Heat index Humidex Humidity Relative humidity ( RH ) Mixing ratio Potential temperature ( θ ) Equivalent potential temperature ( θ ) Sea surface temperature ( SST ) Thermodynamic temperature Vapor pressure Virtual temperature Wet - bulb temperature Wet - bulb potential temperature Wind chill Pressure Atmospheric pressure Baroclinity Barotropicity Pressure gradient Pressure - gradient force ( PGF ) Retrieved from `` https://en.wikipedia.org/w/index.php?title=Dew_point&oldid=813547967 '' Categories : Atmospheric thermodynamics Psychrometrics Threshold temperatures Gases Meteorological data and networks Humidity and hygrometry Hidden categories : Articles needing additional references from October 2016 All articles needing additional references All articles with unsourced statements Articles with unsourced statements from November 2016 Talk Contents About Wikipedia Afrikaans Беларуская Català Чӑвашла Čeština Dansk Deutsch Eesti Español Esperanto فارسی Français Gaeilge Galego 한국어 Հայերեն Hrvatski Italiano עברית Қазақша Kreyòl ayisyen Latviešu Lietuvių Magyar Nederlands 日本 語 Norsk Norsk nynorsk Polski Português Română Русиньскый Русский Simple English Slovenčina Slovenščina کوردی Српски / srpski Srpskohrvatski / српскохрватски Suomi Svenska Türkçe Українська اردو Tiếng Việt 中文 Edit links This page was last edited on 4 December 2017, at 00 : 48. 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Question: relative humidity calculation from dew point and temperature
Answer: high relative humidity implies that the dew point is closer to the current air temperature