@@ -66,69 +66,17 @@ \subsubsection{Heat Index}\label{heat-index}
6666\end {tabular }
6767\end {table }
6868
69- The computation of the heat index is a refinement of a result obtained by
69+ Before version 24.2, the computation of the heat index is a refinement of a result obtained by
7070multiple regression analysis carried out by Lans P. Rothfusz and described in a
71- 1990 National Weather Service (NWS) Technical Attachment (SR 90-23) [4-5]. The
72- calculation is based on degree Fahrenheit.
71+ 1990 National Weather Service (NWS) Technical Attachment (SR 90-23) [4-5].
7372
74- The regression equation of Rothfusz is
75- \begin {equation } \label {eq:rm-1 }
76- HI = c_1 + c_2T + c_3R + c_4TR + c_5T^2 + c_6R^2 + c_7T^2R + c_8TR^2 + c_9T^2R^2
77- \end {equation }
78-
79- where
80-
81- HI = heat index (expressed as an apparent temperature in degrees Fahrenheit),
82-
83- T = ambient dry-bulb temperature (in degrees Fahrenheit),
84-
85- R = relative humidity (percentage value between 0 and 100),
86-
87- $ c_1 $ = -42.379,
88-
89- $ c_2 $ = 2.04901523,
90-
91- $ c_3 $ = 10.14333127,
92-
93- $ c_4 $ = -0.22475541,
94-
95- $ c_5 $ = -0.00683783,
96-
97- $ c_6 $ = -0.05481717,
98-
99- $ c_7 $ = 0.00122874,
100-
101- $ c_8 $ = 0.00085282,
102-
103- $ c_9 $ = -0.00000199.
104-
105- If the RH is less than 13\% and the temperature is between 80 and \IP {112}{\fahrenheit }, then
106- the following adjustment is subtracted from HI:
107-
108- \begin {equation } \label {eq:rm-2 }
109- HI = (13 - R) / 4 * ((17 - |T - 95|) / 17)^{0.5}
110- \end {equation }
111-
112- Otherwise, if the RH is greater than 85\% and the temperature is between 80 and
113- \IP {87}{\fahrenheit }, then the following adjustment is added to HI:
114-
115- \begin {equation } \label {eq:rm-3 }
116- HI = (R - 85) / 10 * (87 - T) / 5
117- \end {equation }
118-
119- The Rothfusz regression is not appropriate when conditions of temperature and
120- humidity warrant a heat index value below about \IP {80}{\fahrenheit }. In those cases, a simpler
121- formula is applied to calculate values consistent with Steadman's results:
122-
123- \begin {equation } \label {eq:rm-4 }
124- HI = 0.5 * (T + 61.0 + (T - 68.0) * 1.2 + (R * 0.094))
125- \end {equation }
126-
127- In practice, the simple formula is computed first based on the temperature and
128- humidity. If this heat index value is \IP {80}{\fahrenheit } or higher, the full regression
129- equation along with any adjustment as described above is applied. The Rothfusz
130- regression is not valid for extreme temperature and relative humidity conditions
131- beyond the range of data considered by Steadman.
73+ Starting from version 24.2, the heat index calculation adopts the extended heat
74+ index method developed by Lu \& Romps [17]. The previous heat index gives
75+ unrealistic results for very hot and humid or very cold and dry conditions. The
76+ extended index extends the domain of the heat index calculation to all
77+ combinations of temperature and relative humidity and gives a more realistic heat
78+ index for the extreme conditions. The implementation in EnergyPlus is based on
79+ the released Python code by Lu and Romps [18].
13280
13381The Heat Index Hours (accumulated hours for a space) and Heat Index
13482OccupantHours (accumulated hours for the sum of all occupants in a space) of
@@ -516,3 +464,11 @@ \subsection{References}
516464
517465{[}16{]} ACGIH, Threshold Limit Values (TLVs) and Biological Exposure Indices
518466(BEIs), 2012. doi:10.1073/pnas.0703993104.
467+
468+ {[}17{]} Lu, Yi-Chuan, and David M. Romps. `` Extending the heat index'' . Journal
469+ of Applied Meteorology and Climatology 61, no. 10 (2022): 1367-1383.
470+ doi:10.1073/pnas.0703993104.
471+
472+ {[}18{]} Lu, Yi-Chuan, and David M. Romps. `` Lu and Romps, Extending the heat index, JAMC, 2022'' ,
473+ Physics of Climate, February 23, 2023.
474+ https://romps.berkeley.edu/papers/pubs-2020-heatindex.html.
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