Fig. 3: Spatial pattern of zonal and meridional advection and respective components. | npj Climate and Atmospheric Science

Fig. 3: Spatial pattern of zonal and meridional advection and respective components.

From: Equatorial convection controls boreal summer intraseasonal oscillations in the present and future climates

Fig. 3

Breakdown of zonal (a–d) and meridional advection (e–h) into the respective components (Eqs. (5) and (6)) for AAPM and BAPM. Stippling represents values significant at 95% using a two-tailed t-test. Contours show the horizontal advection term (L.H.S of Eq. (4)) from −30 to 30 W/m2 in steps of 10. solid contours show a positive tendency and dashed contours show a negative horizontal advection. Refer to Supplementary Fig. 14 for scaled version of the figure.

Back to article page