Figure 4 | Scientific Reports

Figure 4

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

Figure 4

Differences in JAS moisture convergence. (a) \(-\overrightarrow{{V}_{c}}\cdot {\rm{\nabla }}(\delta q)\), (b) \(-(\delta \overrightarrow{V})\cdot {\rm{\nabla }}{q}_{c}\), (c) \(-(\delta {q}_{c})\) \({\rm{\nabla }}\cdot \overrightarrow{{V}_{c}}\), and (d) \(-{q}_{c}\,{\rm{\nabla }}\cdot (\delta \overrightarrow{V})\) between SEN_A and CON. 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.

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