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 | Bibtex)Cite the data
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 )
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 )
Pan-Third Pole Environment Study for a Green Silk Road-A CAS Strategic Priority A Program
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Example of acknowledgement statement is included below: The data set is provided by National Tibetan Plateau Data Center (http://data.tpdc.ac.cn).
License： This work is licensed under an Attribution 4.0 International (CC BY 4.0)
3.HiWATER: Dataset of flux observation matrix (eddy covariance system of Zhangye wetland Station) of the MUlti-Scale Observation EXperiment on Evapotranspiration over heterogeneous land surfaces 2012 (MUSOEXE-12)
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