and North Pacific ocean during winter, when the latent and sensible components are large and the incoming shortwave radiative flux is low.In the North Atlantic and North Pacific (north of about 15°N), flux anomalies are partially caused by local variations in the monthly mean wind direction. ...
The data presented here is a subset of the full ERA5-Land dataset post-processed by ECMWF. Monthly-mean averages have been pre-calculated to facilitate many applications requiring easy and fast access to the data, when sub-monthly fields are not required. Please note that the convention for ...
The data presented here is a subset of the full ERA5-Land dataset post-processed by ECMWF. Monthly-mean averages have been pre-calculated to facilitate many applications requiring easy and fast access to the data, when sub-monthly fields are not required. Please note that the convention for ...
Similarly, clear-sky biases of LST tended to have a relatively significant impact on the error contributions of LST to monthly ET estimation when the climate became humid, with a relatively significant enlarging from −6.3 % in the arid area to −10.0 % in the humid area, especially in ...