Selected article for: "relative humidity and RH relative humidity"
Author: Yueling Ma; Yadong Zhao; Jiangtao Liu; Xiaotao He; Bo Wang; Shihua Fu; Jun Yan; Jingping Niu; Bin Luo
Title: Effects of temperature variation and humidity on the mortality of COVID-19 in Wuhan
  • Document date: 2020_3_18
    • ID: f53i4n02_10
    Snippet: Where e s (T 0 ) denotes saturation vapor pressure at a reference temperature T 0 (273.15 K) which equals to 6.11 mb. L denotes the latent heat of evaporation for water (2257 kJ/kg). R v is the gas constant for water vapor [461.53 J/(kg K)]. T denotes daily ambient temperature (K). Then, VP (Pa) was calculated by combining the e s (T) calculated using Eq. (2) with relative humidity (RH):.....
    Document: Where e s (T 0 ) denotes saturation vapor pressure at a reference temperature T 0 (273.15 K) which equals to 6.11 mb. L denotes the latent heat of evaporation for water (2257 kJ/kg). R v is the gas constant for water vapor [461.53 J/(kg K)]. T denotes daily ambient temperature (K). Then, VP (Pa) was calculated by combining the e s (T) calculated using Eq. (2) with relative humidity (RH):

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