Earth Science Stack Exchange is a question and answer site for those interested in the geology, meteorology, oceanography, and environmental sciences. Join them; it only takes a minute:

Sign up
Here's how it works:
  1. Anybody can ask a question
  2. Anybody can answer
  3. The best answers are voted up and rise to the top

How do I convert specific humidity to relative humidity? What variables are needed (e.g. air temperature, pressure, etc.)?

share|improve this question
up vote 15 down vote accepted

Relative humidity is just $e/e_s$, the ratio of the vapor pressure to saturation vapor pressure or or $w/w_s$, the ratio of mass mixing ratios of water vapor at actual and saturation values. If you have specific humidity, which is the mass mixing ratio of water vapor in air, defined as:

$$ q \equiv \dfrac{m_v}{m_v + m_d} = \dfrac{w}{w+1} \approx w.$$

Relative humidity can be expressed as the ratio of water vapor mixing ratio to saturation water vapor mixing ratio, $w/w_s$, where:

$$ w_s \equiv \dfrac{m_{vs}}{m_d} = \dfrac{e_s R_d}{R_v(p-e_s)} \approx 0.622\dfrac{e_s}{p},$$

and from Clausius-Clapeyron:

$$ e_s(T) = e_{s0}\exp\left[\left(\dfrac{L_v(T)}{R_v}\right)\left(\dfrac{1}{T_0} -\dfrac{1}{T} \right)\right] \approx 611\exp\left(\dfrac{17.67(T-T_0)}{T-29.65}\right).$$

Once you have calculated $w$ and $w_s$ you can obtain the relative humidity as:

$$ RH = 100\dfrac{w}{w_s} \approx 0.263pq\left[\exp\left(\dfrac{17.67(T-T_0)}{T-29.65}\right)\right]^{-1}. $$

You could also calculate $RH = 100(e/e_s)$, but I think since you are starting with $q$ it isn't as straightforward as doing it this way.

Variables used:
$q$ specific humidity or the mass mixing ratio of water vapor to total air (dimensionless)
$m_v$ specific mass of water vapor (kg)
$m_{vs}$ specific mass of water vapor at equilibrium (kg)
$m_d$ specific mass of dry air (kg)
$w$ mass mixing ratio of water vapor to dry air (dimensionless)
$w_s$ mass mixing ratio of water vapor to dry air at equilibrium (dimensionless)
$e_s(T)$ saturation vapor pressure (Pa)
$e_{s0}$ saturation vapor pressure at $T_0$ (Pa)
$R_d$ specific gas constant for dry air (J kg$^{-1}$ K$^{-1}$)
$R_v$ specific gas constant for water vapor (J kg$^{-1}$ K$^{-1}$)
$p$ pressure (Pa)
$L_v(T)$ specific enthalpy of vaporization (J kg$^{-1}$)
$T$ temperature (K)
$T_0$ reference temperature (typically 273.16 K) (K)

share|improve this answer
I think there maybe an error here. $$ e_s(T) \approx 611\exp\left(\dfrac{17.67(T-T_0)}{T-29.65}\right).$$ Shouldn't the 611 be 6.11? In a number of papers I've seen ~6 used here, for eg:…. (eq 2). I don't know where your source is from but using this equation I'm getting results out by an order of 100. I think it should be: $$ RH = 100\dfrac{w}{w_s} \approx 26.3pq\left[\exp\left(\dfrac{17.67(T-T_0)}{T-29.65}\right)\right]^{-1}. $$ – stacey Dec 3 '15 at 14:28
@stacey the 611 value in the equation is in units of Pascals, if you are using 6.11 then you are using hPa or mbar units. Either is correct but you need to be aware of units. 611 Pa = 6.11 hPa = 6.11 mbar. Likewise in the second equation you are giving p in hPa if you are off by a factor of 100. I specified in the post that p was in Pa, so if you use hPa you need to adjust by factor of 100. – casey Dec 3 '15 at 14:31
es(T) isn't dependant on pressure, though. I understand multiplying through by 100 later when calculating RH, but surely es(T) should be 6.11? – stacey Dec 3 '15 at 14:36
@stacey do dimensional analysis on the units in the equation noting that 611 is Pa and 6.11 is hPa and then you'll see the scaling factor of 100 is just a Pa to hPa conversion factor, not some arbitrary number. Note that the exponential is dimensionless so the units of $e_s(T)$ are the units of $e_{s0}$. If you want $e_s(T)$ in hPa, use $e_{s0} $ = 6.11 hPa. – casey Dec 3 '15 at 15:21
Also note in the second equation the units of 0.263 is Pa$^{-1}$, so if you are putting in p in units of hPa you end up with a value of RH in units of "hPa Pa$^{-1}$" which shows you why you end up 100 times off. Lastly, if you are still having problems with this, join chat and we can continue this discussion there. – casey Dec 3 '15 at 15:29

Here is an implementation that I wrote in R (with documentation in the header). In addition to laboriously working through a few textbooks and online references, I have compared the results to a psychrometric chart.

As you have likely noticed, it is a challenge to keep these terms and units straight - I wish I had @casey`s answer then!

##' Convert specific humidity to relative humidity
##' converting specific humidity into relative humidity
##' NCEP surface flux data does not have RH
##' from Bolton 1980 The computation of Equivalent Potential Temperature 
##' \url{}
##' @title qair2rh
##' @param qair specific humidity, dimensionless (e.g. kg/kg) ratio of water mass / total air mass
##' @param temp degrees C
##' @param press pressure in mb
##' @return rh relative humidity, ratio of actual water mixing ratio to saturation mixing ratio
##' @export
##' @author David LeBauer
qair2rh <- function(qair, temp, press = 1013.25){
    es <-  6.112 * exp((17.67 * temp)/(temp + 243.5))
    e <- qair * press / (0.378 * qair + 0.622)
    rh <- e / es
    rh[rh > 1] <- 1
    rh[rh < 0] <- 0

Similar variable conversion functions can be found in the metutils.R file in the PEcAn data.atmosphere library.

share|improve this answer

I can't do, or won't do the math, but here is how I get around it. Look up the saturation line at the temperature and pressure that I am concerned with on pseudo-adiabatic diagram. Then multiply the relative humidity times the saturation rate at that temperature. It's not precise, since there are many factors that vary, and you are approximating from a paper chart, but it's a good enough estimate for my work. Hope this is helpful for those of us at the simple end of the concept.

share|improve this answer

Your Answer


By posting your answer, you agree to the privacy policy and terms of service.

Not the answer you're looking for? Browse other questions tagged or ask your own question.