Improving representation of canopy temperatures for modeling subcanopy incoming longwave radiation to the snow surface. Issue 17 (7th September 2017)

• Record Type: Journal Article
• Authors: Webster, Clare; Rutter, Nick; Jonas, Tobias
• Is Part Of: Journal of geophysical research. Volume 122:Issue 17(2017)
• Page Start: 9154
• Page End: 9172
• Publication Date: 2017-09-07
• Subjects: longwave radiation -- thermal infrared imagery -- canopy radiation transfer -- forest canopy structure -- canopy temperatures; Atmospheric physics -- Periodicals; Geophysics -- Periodicals; 551.5
• DOI: 10.1002/2017JD026581
• Languages: English
• ISSNs: 2169-897X

Abstract

Abstract: A comprehensive analysis of canopy surface temperatures was conducted around a small and large gap at a forested alpine site in the Swiss Alps during the 2015 and 2016 snowmelt seasons (March–April). Canopy surface temperatures within the small gap were within 2–3°C of measured reference air temperature. Vertical and horizontal variations in canopy surface temperatures were greatest around the large gap, varying up to 18°C above measured reference air temperature during clear‐sky days. Nighttime canopy surface temperatures around the study site were up to 3°C cooler than reference air temperature. These measurements were used to develop a simple parameterization for correcting reference air temperature for elevated canopy surface temperatures during (1) nighttime conditions (subcanopy shortwave radiation is 0 W m −2 ) and (2) periods of increased subcanopy shortwave radiation >400 W m −2 representing penetration of shortwave radiation through the canopy. Subcanopy shortwave and longwave radiation collected at a single point in the subcanopy over a 24 h clear‐sky period was used to calculate a nighttime bulk offset of 3°C for scenario 1 and develop a multiple linear regression model for scenario 2 using reference air temperature and subcanopy shortwave radiation to predict canopy surface temperature with a root‐mean‐square error (RMSE) of 0.7°C. Outside of these two scenarios, reference air temperature was used to predict subcanopy incoming longwave radiation. Modeling at 20 radiometer locations throughout two snowmelt seasons using these parameterizations reduced the mean bias and RMSE to below 10 W m s −2 at all locations. Key Points: Canopy temperatures around large gaps vary up to 18°C above air temperature during daytime clear‐sky conditions A correction parameterization was developed to estimate canopy temperatures using air temperature and shortwave radiation Mean bias and RMSE could be considerably reduced at 20 radiometer locations during two snowmelt seasons using the new model