4.7 Article

Assessment of gridded datasets of various near surface temperature variables over Heihe River Basin: Uncertainties, spatial heterogeneity and clear-sky bias

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DOI: 10.1016/j.jag.2023.103347

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Temperature; Near surface temperature; Land surface temperature; Air temperature; Soil temperature; Validation; Spatial heterogeneity; Clear -sky bias

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This study evaluated nine gridded near-surface temperature products and analyzed their spatial heterogeneity and clear-sky bias using extensive measurements collected at Heihe River Basin. The MXD21 product had the lowest root mean square error (RMSE) but a high percentage of missing values. All-weather skin temperature products showed comparable accuracy for cloudy-sky and clear-sky cases. AMSR2 had the lowest RMSE for air temperature, but a high percentage of invalid data, while ERA5 had a worse accuracy but high spatial resolution and gap-free data coverage. Soil and air temperatures had higher accuracies than skin temperature, and different variables showed variations in spatiotemporal heterogeneity and clear-sky biases.
Near-surface temperatures, such as air, land surface, and soil temperatures, play significant roles in surface ra-diation and energy balance. This study assessed nine gridded near-surface temperature products and analyzed the spatial heterogeneity and clear-sky bias of these temperature variables, using extensive measurements collected at Heihe River Basin. The MXD21 (MOD21 and MYD21) product had the lowest root mean square error (RMSE) (3.35 K) among all skin temperature products but a high percentage of missing values (48.4 %). All-weather skin temperature products had comparable accuracy for the interpolated cloudy-sky cases (RMSE 4.92 K) and observed clear-sky pixels (RMSE 3.42 K). For air temperature, AMSR2 had the lowest RMSE (2.48 K), but a high percentage of invalid data (32.5 %); and ERA5 had a worse accuracy (RMSE 3.87 K) but a high spatial resolution and gap-free data coverage. Comparing products from the same data source, air and soil temperatures had higher accuracies than skin temperature. Among the different variables of temperature, the 0 cm soil temperature and skin temperature had higher spatiotemporal heterogeneity than the air temperature and the soil temperatures at greater depths. The skin temperature, 0 cm soil temperature, and air temperature had higher clear-sky biases compared to soil temperatures.

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