TY - JOUR
T1 - Improved methods for estimating mean radiant temperature in hot and sunny outdoor settings
AU - Vanos, Jennifer K.
AU - Rykaczewski, Konrad
AU - Middel, Ariane
AU - Vecellio, Daniel J.
AU - Brown, Robert D.
AU - Gillespie, Terry J.
N1 - Funding Information:
We would like to express our gratitude to Scott Krayenhoff for aiding in the sensor setup, Paul Coseo for helping with roof access, and Liping Wang, Linshuang Long, and Rajagopalan Ramesh of ASU for help with the FTIR measurements.
Funding Information:
Meteorological sensors were sponsored by University of Kaiserslautern, grant “Microclimate Data Collection, Analysis, and Visualization”.
Publisher Copyright:
© 2021, ISB.
PY - 2021/6
Y1 - 2021/6
N2 - Thermal comfort research has utilized various sensors and models to estimate the mean radiant temperature (MRT) experienced by a human, including the standard black globe thermometer (SGT), acrylic globe thermometers (AGT), and cylindrical radiation thermometers (CRT). Rather than directly measuring radiation, a temperature is measured in the center of these low-cost sensors that can be related to MRT after theoretically accounting for convection. However, these sensors have not been systematically tested under long-term hot and clear conditions. Further, under variable weather conditions, many issues can arise due to slow response times, shape, inaccuracies in material properties and assumptions, and color (albedo, emissivity) inconsistencies. Here, we assess the performance of MRT produced by various heat transfer models, with and without new average surface temperature (T¯ s) correction factors, using five instruments—the SGT (15 cm, black), tan and black CRTs, gray and black 38 mm AGTs—compared to 3D integral radiation measurements. Measurements were taken on an unobscured roof throughout summer-to-early-fall months in Tempe, Arizona, examining 58 full-sun days. Deviations without correcting for asymmetrical surface heating—found to be the main cause of errors—reached ± 15–20 °C MRT. By accounting for asymmetric heating through T¯ s calculations, new corrective algorithms were derived for the low-cost sensor models. Results show significant improvements in the estimated MRT error for each sensor (i.e., ∆MRTmodel − IRM) when applying the T¯ s corrections. The tan MRTCRT improved from 1.9 ± 6.2 to −0.1 ± 4.4 °C, while the gray AGT and SGT showed improvements from −1.6 ± 7.2 to −0.4 ± 6.3 °C and − 6.6 ± 6.4 to − 0.03 ± 5.7 °C, respectively. The new corrections also eliminated dependence on other meteorological factors (zenith, wind speed). From these results, we provide three simple equations for CRT, AGT, and SGT correction for future research use under warm-hot and clear conditions. This study is the most comprehensive empirical assessment of various low-cost instruments with broad applicability in urban climate and biometeorological research.
AB - Thermal comfort research has utilized various sensors and models to estimate the mean radiant temperature (MRT) experienced by a human, including the standard black globe thermometer (SGT), acrylic globe thermometers (AGT), and cylindrical radiation thermometers (CRT). Rather than directly measuring radiation, a temperature is measured in the center of these low-cost sensors that can be related to MRT after theoretically accounting for convection. However, these sensors have not been systematically tested under long-term hot and clear conditions. Further, under variable weather conditions, many issues can arise due to slow response times, shape, inaccuracies in material properties and assumptions, and color (albedo, emissivity) inconsistencies. Here, we assess the performance of MRT produced by various heat transfer models, with and without new average surface temperature (T¯ s) correction factors, using five instruments—the SGT (15 cm, black), tan and black CRTs, gray and black 38 mm AGTs—compared to 3D integral radiation measurements. Measurements were taken on an unobscured roof throughout summer-to-early-fall months in Tempe, Arizona, examining 58 full-sun days. Deviations without correcting for asymmetrical surface heating—found to be the main cause of errors—reached ± 15–20 °C MRT. By accounting for asymmetric heating through T¯ s calculations, new corrective algorithms were derived for the low-cost sensor models. Results show significant improvements in the estimated MRT error for each sensor (i.e., ∆MRTmodel − IRM) when applying the T¯ s corrections. The tan MRTCRT improved from 1.9 ± 6.2 to −0.1 ± 4.4 °C, while the gray AGT and SGT showed improvements from −1.6 ± 7.2 to −0.4 ± 6.3 °C and − 6.6 ± 6.4 to − 0.03 ± 5.7 °C, respectively. The new corrections also eliminated dependence on other meteorological factors (zenith, wind speed). From these results, we provide three simple equations for CRT, AGT, and SGT correction for future research use under warm-hot and clear conditions. This study is the most comprehensive empirical assessment of various low-cost instruments with broad applicability in urban climate and biometeorological research.
KW - Absorbed radiation
KW - Cylindrical radiation thermometer
KW - Extreme heat
KW - Globe thermometer
KW - Mean radiant temperature
KW - Radiation geometry
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U2 - 10.1007/s00484-021-02131-y
DO - 10.1007/s00484-021-02131-y
M3 - Article
C2 - 33909138
AN - SCOPUS:85105421826
SN - 0020-7128
VL - 65
SP - 967
EP - 983
JO - International Journal of Biometeorology
JF - International Journal of Biometeorology
IS - 6
ER -