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  2. Vapour-pressure deficit - Wikipedia

    en.wikipedia.org/wiki/Vapour-pressure_deficit

    Global distribution of Vapour-pressure deficit averaged over the years 1981-2010 from the CHELSA-BIOCLIM+ data set [1] Vapour pressure-deficit, or VPD, is the difference (deficit) between the amount of moisture in the air and how much moisture the air can hold when it is saturated. Once air becomes saturated, water will condense to form clouds ...

  3. Vapor pressure - Wikipedia

    en.wikipedia.org/wiki/Vapor_pressure

    Vapor pressure [a] or equilibrium vapor pressure is the pressure exerted by a vapor in thermodynamic equilibrium with its condensed phases (solid or liquid) at a given temperature in a closed system. The equilibrium vapor pressure is an indication of a liquid's thermodynamic tendency to evaporate.

  4. Penman–Monteith equation - Wikipedia

    en.wikipedia.org/wiki/Penman–Monteith_equation

    δe = vapor pressure deficit (Pa) g a = Conductivity of air, atmospheric conductance (m s −1) g s = Conductivity of stoma, surface or stomatal conductance (m s −1) γ = Psychrometric constant (γ ≈ 66 Pa K −1) Note: Often, resistances are used rather than conductivities.

  5. Global Warming Is Drying Out Fire Fuels - AOL

    www.aol.com/global-warming-drying-fire-fuels...

    A UCLA professor used artificial intelligence to study wildfire data, focusing on vapor pressure deficit. Wildfires ravaged the western United States this year, with some of the biggest fires in ...

  6. Tetens equation - Wikipedia

    en.wikipedia.org/wiki/Tetens_equation

    where temperature T is in degrees Celsius (°C) and saturation vapor pressure P is in kilopascals (kPa). According to Monteith and Unsworth, "Values of saturation vapour pressure from Tetens' formula are within 1 Pa of exact values up to 35 °C." Murray (1967) provides Tetens' equation for temperatures below 0 °C: [3]

  7. Potential evapotranspiration - Wikipedia

    en.wikipedia.org/wiki/Potential_evapotranspiration

    δe = vapor pressure deficit (kPa) γ = Psychrometric constant (γ ≈ 66 Pa K −1) N.B.: The coefficients 0.408 and 900 are not unitless but account for the conversion from energy values to equivalent water depths: radiation [mm day −1] = 0.408 radiation [MJ m −2 day −1].

  8. Virtual temperature - Wikipedia

    en.wikipedia.org/wiki/Virtual_temperature

    In atmospheric thermodynamics, the virtual temperature of a moist air parcel is the temperature at which a theoretical dry air parcel would have a total pressure and density equal to the moist parcel of air. [1]

  9. Michigan athletic director Warde Manuel gets 5-year contract ...

    www.aol.com/michigan-athletic-director-warde...

    Michigan gave athletic director Warde Manuel a five-year contract extension Thursday on the heels of the Wolverines' upset over rival Ohio State and a strong start to the basketball season.