import numpy as np
import logging
"""
Calculate the saturation vapor pressure
Example: Calculate the vapor pressure over liquid water using the WMO
formula
temp = FINDGEN(100) - 100.
P = VaporPressure(temp, 'liquid', 'WMO')
For temperatures above 0 deg C the vapor pressure over liquid water
is calculated.
The optional parameter 'liquid' changes the calculation to vapor pressure
over liquid water over the entire temperature range.
The formula to be used can be selected with the appropriate keyword
The current default fomulas are Hyland and Wexler for liquid and
Goff Gratch for ice.
Parameters
----------
temp : float
Temperature in [deg C]
phase : str
'liquid' : Calculate vapor pressure over liqiud water or
'ice' : Calculate vapor pressure over ice
meth : str
formula to be used
MartiMauersberger : vaporpressure formula from Marti Mauersberger
MagnusTetens : vaporpressure formula from Magnus Tetens
GoffGratch : vaporpressure formula from Goff Gratch
Buck_original : vaporpressure formula from Buck (original)
Buck_manual : vaporpressure formula from the Buck manual
CIMO : vaporpressure formula recommended by CIMO
Vaisala : vaporpressure formula from Vaisala
WMO_Goff : vaporpressure formula from WMO, which should have been Goff
WMO2000 : vaporpressure formula from WMO (2000) containing a typo
Wexler : vaporpressure formula from Wexler (1976)
Sonntag : vaporpressure formula from Sonntag (1994)
Bolton : vaporpressure formula from Bolton (1980)
HylandWexler : vaporpressure formula from Hyland and Wexler (1983)
IAPWS : vaporpressure formula from IAPWS (2002)
Preining : vaporpressure formula from Preining (2002)
MurphyKoop : vaporpressure formula from Murphy and Koop (2005)
Returns
-------
P : float
Saturation vapor pressure in [hPa]
Author
------
Holger Voemel
NCAR / EOL
PO BOX 3000
Boulder, CO 80303
USA
Ported to Python and modified by S. Biri
COPYRIGHT
---------
Copyright (c) 2015, Holger Voemel
"""
def VaporPressure(temp, P, phase, meth):
logging.basicConfig(filename='VaporPressure.log',
format='%(asctime)s %(message)s',level=logging.info)
Psat = np.zeros(temp.size)*np.nan
if (np.nanmin(temp) > 200): # if Ta in Kelvin convert to Celsius
temp = temp-273.16
T = np.copy(temp)+273.16 # Most formulas use T in [K]
# Formulas using [C] use the variable temp
# Default uses Hyland and Wexler over liquid. While this may not be
# the best formula, it is consistent with what Vaisala uses in their
# system
# Calculate saturation pressure over liquid water
if (phase == 'liquid'):
if (meth == 'HylandWexler' or meth == ''):
logging.info("Source Hyland, R. W. and A. Wexler, Formulations \
for the Thermodynamic Properties of the saturated \
Phases of H2O from 173.15K to 473.15K, \
ASHRAE Trans, 89(2A), 500-519, 1983.")
Psat = np.exp(-0.58002206e4/T+0.13914993e1-0.48640239e-1*T +
0.41764768e-4*np.power(T, 2) -
0.14452093e-7*np.power(T, 3) +
0.65459673e1*np.log(T))/100
if (meth == 'Hardy'):
logging.info("Source Hardy, B., 1998, ITS-90 Formulations \
for Vapor Pressure, Frostpoint Temperature, \
Dewpoint Temperature, and Enhancement Factors \
in the Range -100 to +100°C, The Proceedings of \
the Third International Symposium on Humidity & \
Moisture, London, England")
Psat = np.exp(-2.8365744e3/np.power(T, 2)-6.028076559e3/T +
1.954263612e1-2.737830188e-2*T +
1.6261698e-5*np.power(T, 2) +
7.0229056e-10*np.power(T, 3) -
1.8680009e-13*np.power(T, 4) +
2.7150305*np.log(T))/100
if (meth == 'Preining'):
logging.info("Source : Vehkamaeki, H., M. Kulmala, I. Napari, \
K. E. J. Lehtinen, C.Timmreck, M. Noppel, and \
A. Laaksonen (2002), J. Geophys. Res., 107, \
doi:10.1029/2002JD002184.")
Psat = np.exp(-7235.424651/T+77.34491296+5.7113e-3*T -
8.2*np.log(T))/100
if (meth == 'Wexler'):
logging.info("Wexler, A., Vapor Pressure Formulation for Water \
in Range 0 to 100 C. A Revision, Journal of Research \
of the National Bureau of Standards - A. Physics and \
Chemistry, September - December 1976, Vol. 80A, \
Nos.5 and 6, 775-785")
Psat = np.exp(-0.29912729e4*np.power(T, -2) -
0.60170128e4*np.power(T, -1) +
0.1887643854e2-0.28354721e-1*T +
0.17838301e-4*np.power(T, 2) -
0.84150417e-9*np.power(T, 3) +
0.44412543e-12*np.power(T, 4) + # This line was corrected from '-' to '+' following the original citation. (HV 20140819). The change makes only negligible difference
2.858487*np.log(T))/100
if ((meth == 'GoffGratch') or (meth == 'MartiMauersberger')):
# logging.info("Marti and Mauersberger don't have a vapor pressure \
# curve over liquid. Using Goff Gratch instead; \
# Goff Gratch formulation Source : Smithsonian \
# Meteorological Tables, 5th edition, p. 350, 1984 \
# From original source: Goff & Gratch (1946), p. 107) \
# Goff Gratch formulation; Source : Smithsonian \
# Meteorological Tables, 5th edition, p. 350, 1984 \
# From original source: Goff and Gratch (1946), p. 107")
Ts = 373.16 # steam point temperature in K
ews = 1013.246 # saturation pressure at steam point temperature
Psat = np.power(10, -7.90298*(Ts/T-1)+5.02808*np.log10(Ts/T) -
1.3816e-7*(np.power(10, 11.344*(1-T/Ts))-1) +
8.1328e-3*(np.power(10, -3.49149*(Ts/T-1))-1) +
np.log10(ews))
if (meth == 'CIMO'):
logging.info("Source: Annex 4B, Guide to Meteorological \
Instruments and Methods of Observation, \
WMO Publication No 8, 7th edition, Geneva, 2008. \
(CIMO Guide)")
Psat = (6.112*np.exp(17.62*temp/(243.12+temp)) *
(1.0016+3.15e-6*P-0.074/P))
if (meth == 'MagnusTetens'):
logging.info("Source: Murray, F. W., On the computation of \
saturation vapor pressure, J. Appl. Meteorol., \
6, 203-204, 1967.")
Psat = np.power(10, 7.5*(temp)/(temp+237.5)+0.7858)
# Murray quotes this as the original formula and
Psat = 6.1078*np.exp(17.269388*temp/(temp+237.3))
# this as the mathematical aquivalent in the form of base e.
if (meth == 'Buck'):
logging.info("Bucks vapor pressure formulation based on \
Tetens formula. Source: Buck, A. L., \
New equations for computing vapor pressure and \
enhancement factor, J. Appl. Meteorol., 20, \
1527-1532, 1981.")
Psat = (6.1121*np.exp(17.502*temp/(240.97+temp)) *
(1.0007+(3.46e-6*P)))
if (meth == 'Buck2'):
logging.info("Bucks vapor pressure formulation based on \
Tetens formula. Source: Buck Research, \
Model CR-1A Hygrometer Operating Manual, Sep 2001")
Psat = (6.1121*np.exp((18.678-(temp)/234.5)*(temp)/(257.14+temp)) *
(1+1e-4*(7.2+P*(0.0320)+5.9e-6*np.power(T, 2))))
if (meth == 'WMO'):
logging.info("Intended WMO formulation, originally published by \
Goff (1957) incorrectly referenced by WMO technical \
regulations, WMO-NO 49, Vol I, General \
Meteorological Standards and Recommended Practices, \
App. A, Corrigendum Aug 2000. and incorrectly \
referenced by WMO technical regulations, \
WMO-NO 49, Vol I, General Meteorological Standards \
and Recommended Practices, App. A, 1988.")
Ts = 273.16 # triple point temperature in K
Psat = np.power(10, 10.79574*(1-Ts/T)-5.028*np.log10(T/Ts) +
1.50475e-4*(1-np.power(10, -8.2969*(T/Ts-1))) +
0.42873e-3*(np.power(10, -4.76955*(1-Ts/T))-1) +
0.78614)
if (meth == 'WMO2000'):
logging.info("WMO formulation, which is very similar to Goff \
Gratch. Source : WMO technical regulations, \
WMO-NO 49, Vol I, General Meteorological Standards \
and Recommended Practices, App. A, \
Corrigendum Aug 2000.")
Ts = 273.16 # triple point temperature in K
Psat = np.power(10, 10.79574*(1-Ts/T)-5.028*np.log10(T/Ts) +
1.50475e-4*(1-np.power(10, -8.2969*(T/Ts-1))) +
0.42873e-3*(np.power(10, -4.76955*(1.-Ts/T))-1) +
0.78614)
if (meth == 'Sonntag'):
logging.info("Source: Sonntag, D., Advancements in the field of \
hygrometry, Meteorol. Z., N. F., 3, 51-66, 1994.")
Psat = np.exp(-6096.9385*np.power(T, -1)+16.635794 -
2.711193e-2*T+1.673952e-5*np.power(T, 2) +
2.433502*np.log(T))#*(1.0016+P*3.15e-6-0.074/P)
if (meth == 'Bolton'):
logging.info("Source: Bolton, D., The computation of equivalent \
potential temperature, Monthly Weather Report, 108, \
1046-1053, 1980. equation (10)")
Psat = 6.112*np.exp(17.67*temp/(temp+243.5))
if (meth == 'IAPWS'):
logging.info("Source: Wagner W. and A. Pruss (2002), The IAPWS \
formulation 1995 for the thermodynamic properties \
of ordinary water substance for general and \
scientific use, J. Phys. Chem. Ref. Data, 31(2), \
387-535. This is the 'official' formulation from \
the International Association for the Properties of \
Water and Steam The valid range of this formulation \
is 273.16 <= T <= 647.096 K and is based on the \
ITS90 temperature scale.")
Tc = 647.096 # K : Temperature at the critical point
Pc = 22.064e4 # hPa : Vapor pressure at the critical point
nu = (1-T/Tc)
a1, a2, a3 = -7.85951783, 1.84408259, -11.7866497
a4, a5, a6 = 22.6807411, -15.9618719, 1.80122502
Psat = (Pc*np.exp(Tc/T*(a1*nu+a2*np.power(nu, 1.5) +
a3*np.power(nu, 3)+a4*np.power(nu, 3.5) +
a5*np.power(nu, 4)+ a6*np.power(nu, 7.5))))
if (meth == 'MurphyKoop'):
logging.info("Source : Murphy and Koop, Review of the vapour \
pressure of ice and supercooled water for \
atmospheric applications, Q. J. R. Meteorol. \
Soc (2005), 131, pp. 1539-1565.")
Psat = np.exp(54.842763-6763.22/T-4.210*np.log(T)+0.000367*T +
np.tanh(0.0415*(T-218.8))*(53.878-1331.22/T -
9.44523*np.log(T)+0.014025*T))/100
# Calculate saturation pressure over ice ----------------------------------
elif (phase == 'ice'):
logging.info("Default uses Goff Gratch over ice. There is little \
ambiguity in the ice saturation curve. Goff Gratch \
is widely used.")
if (meth == 'MartiMauersberger'):
logging.info("Source : Marti, J. and K Mauersberger, A survey and \
new measurements of ice vapor pressure at \
temperatures between 170 and 250 K, GRL 20, \
363-366, 1993.")
Psat = np.power(10, -2663.5/T+12.537)/100
if (meth == 'HylandWexler'):
logging.info("Source Hyland, R. W. and A. Wexler, Formulations \
for the Thermodynamic Properties of the saturated \
Phases of H2O from 173.15K to 473.15K, ASHRAE Trans,\
89(2A), 500-519, 1983.")
Psat = np.exp(-0.56745359e4/T+0.63925247e1-0.96778430e-2*T +
0.62215701e-6*np.power(T, 2) +
0.20747825e-8*np.power(T, 3) -
0.9484024e-12*np.power(T, 4) +
0.41635019e1*np.log(T))/100
if (meth == 'Wexler'):
logging.info("Wexler, A., Vapor pressure formulation for ice, \
Journal of Research of the National Bureau of \
Standards-A. 81A, 5-20, 1977.")
Psat = np.exp(-0.58653696e4*np.power(T, -1)+0.22241033e2 +
0.13749042e-1*T-0.34031775e-4*np.power(T, 2) +
0.26967687e-7*np.power(T, 3) +
0.6918651*np.log(T))/100
if (meth == 'Hardy'):
logging.info("Source Hardy, B., 1998, ITS-90 Formulations for \
Vapor Pressure, Frostpoint Temperature, Dewpoint \
Temperature, and Enhancement Factors in the Range \
-100 to +100°C, The Proceedings of the Third \
International Symposium on Humidity & Moisture, \
London, England. These coefficients are updated to \
ITS90 based on the work by Bob Hardy at Thunder \
Scientific: http://www.thunderscientific.com/\
tech_info/reflibrary/its90formulas.pdf \
The difference to the older ITS68 coefficients used \
by Wexler is academic.")
Psat = np.exp(-0.58666426e4*np.power(T, -1)+0.2232870244e2 +
0.139387003e-1*T-0.34262402e-4*np.power(T, 2) +
0.27040955e-7*np.power(T, 3) +
0.67063522e-1*np.log(T))/100
if (meth == 'GoffGratch' or meth == '' or meth == 'IAPWS'):
logging.info("IAPWS does not provide a vapor pressure formulation \
over ice use Goff Gratch instead.\
Source : Smithsonian Meteorological Tables, \
5th edition, p. 350, 1984")
ei0 = 6.1071 # mbar
T0 = 273.16 # triple point in K
Psat = np.power(10, -9.09718*(T0/T-1)-3.56654*np.log10(T0/T) +
0.876793*(1-T/T0)+np.log10(ei0))
if (meth == 'MagnusTetens'):
logging.info("Source: Murray, F. W., On the computation of \
saturation vapor pressure, J. Appl. Meteorol., 6, \
203-204, 1967.")
Psat = np.power(10, 9.5*temp/(265.5+temp)+0.7858)
# Murray quotes this as the original formula and
Psat = 6.1078*np.exp(21.8745584*(T-273.16)/(T-7.66))
# this as the mathematical aquivalent in the form of base e.
if (meth == 'Buck'):
logging.info("Bucks vapor pressure formulation based on Tetens \
formula. Source: Buck, A. L., New equations for \
computing vapor pressure and enhancement factor, \
J. Appl. Meteorol., 20, 1527-1532, 1981.")
Psat = (6.1115*np.exp(22.452*temp/(272.55+temp)) *
(1.0003+(4.18e-6*P)))
if (meth == 'Buck2'):
logging.info("Bucks vapor pressure formulation based on Tetens \
formula. Source: Buck Research, Model CR-1A \
Hygrometer Operating Manual, Sep 2001")
Psat = (6.1115*np.exp((23.036-temp/333.7)*temp/(279.82+temp)) *
(1+1e-4*(2.2+P*(0.0383+6.4e-6*np.power(T, 2)))))
if (meth == 'CIMO'):
logging.info("Source: Annex 4B, Guide to Meteorological \
Instruments and Methods of Observation, \
WMO Publication No 8, 7th edition, Geneva, 2008. \
(CIMO Guide)")
Psat = (6.112*np.exp(22.46*temp/(272.62+temp)) *
(1.0016+3.15e-6*P-0.074/P))
if (meth == 'WMO' or meth == 'WMO2000'):
logging.info("There is no typo issue in the WMO formulations for \
ice. WMO formulation, which is very similar to Goff \
Gratch. Source : WMO technical regulations, \
WMO-NO 49, Vol I, General Meteorological Standards \
and Recommended Practices, Aug 2000, App. A.")
T0 = 273.16 # triple point temperature in K
Psat = np.power(10, -9.09685*(T0/T-1)-3.56654*np.log10(T0/T) +
0.87682*(1-T/T0)+0.78614)
if (meth == 'Sonntag'):
logging.info("Source: Sonntag, D., Advancements in the field of \
hygrometry, Meteorol. Z., N. F., 3, 51-66, 1994.")
Psat = np.exp(-6024.5282*np.power(T, -1)+24.721994+1.0613868e-2*T -
1.3198825e-5*np.power(T, 2)-0.49382577*np.log(T))
if (meth == 'MurphyKoop'):
logging.info("Source : Murphy and Koop, Review of the vapour \
pressure of ice and supercooled water for \
atmospheric applications, Q. J. R. Meteorol. Soc \
(2005), 131, pp. 1539-1565.")
Psat = np.exp(9.550426-5723.265/T+3.53068*np.log(T) -
0.00728332*T)/100
s = np.where(temp > 0)
if (s.size[0] >= 1):
logging.info("Independent of the formula used for ice, use \
Hyland Wexler (water) for temperatures above freezing\
(see above). Source Hyland, R. W. and A. Wexler, \
Formulations for the Thermodynamic Properties of the \
saturated Phases of H2O from 173.15K to 473.15K, \
ASHRAE Trans, 89(2A), 500-519, 1983.")
Psat_w = np.exp(-0.58002206e4/T+0.13914993e1-0.48640239e-1*T +
0.41764768e-4*np.power(T, 2) -
0.14452093e-7*np.power(T, 3) +
0.65459673e1*np.log(T))/100
Psat[s] = Psat_w[s]
return Psat