Figure 3 | Scientific Reports

Figure 3

From: Influence of Latent Heating over the Asian and Western Pacific Monsoon Region on Sahel Summer Rainfall

Figure 3

Differences in JAS omega, zonal wind, meridional wind, and water vapor flux. Differences in JAS (a) omega, zonal wind (vector) and meridional wind (shading) at 14.2°N between SEN_A and CON, and (b) water vapor flux (vector) and its divergence (shading) at 900 hPa between SEN_E and CON. The meridional wind and vectors denote the regions where the changes are statistically significant at the 95% confidence level according to the t-test. Omega is scaled so that the vertical motion is visible. This figure was generated by the NCAR Command Language (Version 6.3.0) [Software]. (2016). Boulder, Colorado: UCAR/NCAR/CISL/TDD. http://dx.doi.org/10.5065/D6WD3XH5.

Back to article page