Two types of simulations are designed (i.e., B case and H case). For each type, four simulations are performed with different heterogeneity length scales (e.g., 2000 m, 1200 m, 550 m and 240 m). Hence, the first char of the filename in our dateset refers to the simulation type and the following numbers represent the heterogeneity length scales.
1. Zhou, Y.Z., Li, D., Li, X. (2019). The Effects of Surface Heterogeneity Scale on the Flux Imbalance under Free Convection, Journal of Geophysical Research: Atmospheres, doi:10.1029/2018jd029550.( View Details | Download )Cite the data
ZHOU Yanzhao. The Surface Heterogeneity patterns and the Flux Imbalance under Free Convection based on the WRF LES. Big Data System for Pan-Third Pole, 2019. doi: 10.11888/Meteoro.tpdc.270103. (Download the reference： RIS | Bibtex )
Using this data, you must reference article references listed in the Required Data Citation and reference data
1.Zhou, Y.Z., Li, D., Liu, H. and Li, X., (2018). Diurnal variations of the flux imbalance over homogeneous and heterogeneous landscapes. Boundary Layer Meteorol. 168(3), 417-442. doi:10.1007/s10546-018-0358-2. (View Details | Download )
Pan-Third Pole Environment Study for a Green Silk Road-A CAS Strategic Priority A Program
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1. HiWATER: The Multi-Scale Observation Experiment on Evapotranspiration over heterogeneous land surfaces (MUSOEXE) Dataset - flux observation matrix (an eddy covariance system at Zhangye wetland Station)
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