4.7 Article

Global estimates of 500 m daily aerodynamic roughness length from MODIS data

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DOI: 10.1016/j.isprsjprs.2021.11.015

关键词

Aerodynamic roughness length; Machine learning; MODIS; Evapotranspiration

资金

  1. National Key R&D Program of China [2018YFA0605401]
  2. National Natural Science Foundation of China [41922009, 42071332]

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This study presented a practical method for global estimates of 500m daily z0(m) using machine learning techniques, wind profile equation, observations, and MODIS data. The random forest model outperformed deep neural network and convolutional neural network models, showing high accuracy in reproducing daily z0(m) across all land cover types. These results can assist in improving the simulation of momentum, water, and energy transfer between land and atmosphere, enhancing the development of high-resolution land surface and Earth system models.
Aerodynamic roughness length (z0(m)) is a key parameter in the characterization of land surface turbulent heat fluxes and widely used in many surface and climate-related process models. The global products of time series of z0m at finer spatio-temporal resolution, however, have never been publicly available. Here we presented a practical method for global estimates of 500 m daily z0(m) with a combination of machine learning techniques, wind profile equation, observations from 273 sites and MODIS remote sensing data. Results showed that the random forest (RF) model outperformed the deep neural network (DNN) and convolutional neural network (CNN) models, and it could well reproduce the magnitude and temporal variability of daily z0(m) at almost all sites for all land cover types. In the validation of the RF-estimated daily z0(m) with the in-situ observations, the root mean square error (RMSE) varied between 0.02 m and 0.09 m, the mean absolute error (MAE) varied between 0.01 m and 0.05 m and the coefficient of determination (R2) was 1 for medium-to-high canopy shrublands, savannas and forests; for short-canopy croplands, grasslands and wetlands, the RMSE and MAE were 0.02 m and 0.01 m, respectively, and the R2 varied between 0.94 and 1. Compared to the Climate Forecast System Version 2 (CFSv2, 0.3/monthly) and ECMWF Reanalysis v5 (ERA5, 0.25/monthly) products in 2019, the RF-estimated z0m was found to have the similar global spatial pattern but significantly larger temporal variability, and it also showed a higher and lower global mean of z0(m) over forests and non-forests, respectively. The RF-estimated z0(m) displayed a higher temporal variability but a similar global spatial pattern of this variability compared to the CFSv2, whereas the ERA5 z0m product exhibited almost no temporal variability except for grasslands and croplands. This study is beneficial for improving the simulation of the momentum, water and energy transfer between land and atmosphere and helping boost the development of high-resolution land surface models and Earth system models.

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