Characteristics of Thermally-Induced Near-Surface Flows over An Enclosed Crater: Observations of the Meteor Crater Experiment (METCRAX)

WANG Lin-Lin, GUO Xiao-Feng, WAN Bing-Cheng

Figure 2 Wind frequency distributions by means of a, b wind roses and c, d histograms separately for the daytime, 0600-1800 MST Mountain Standard Time, and the nighttime, 1800-0600 MST. See Table 1 for information about the different measurement sites.