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.
ZHOU Yanzhao. The surface heterogeneity patterns and the flux Imbalance under free convection based on the WRF LES. National Tibetan Plateau Data Center, 2019. doi: 10.11888/Meteoro.tpdc.270103. (Download the reference： RIS | Bibtex )Related Literatures:
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 | Bibtex)
2. 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 | Bibtex)
Using this data, the data citation is required to be referenced and the related literatures are suggested to be cited.
Pan-Third Pole Environment Study for a Green Silk Road-A CAS Strategic Priority A Program (No:XDA20000000)
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