‘A mess’ and ‘rows’: evaluation in prime-time TV news by MARIANNA PATRONA


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2(c) that the regions of low-level convergence and upper-level divergence are those of dense clouding and heavy precipitation (as shown by hatching below the bottom line in the lower panel) and where they diverge at low levels and converge aloft are relatively cloud-free areas with little or no precipitation. According to observations, heavy clouding and precipitation occur along the equator in some preferred regions, such as equatorial Eastern Indian Ocean, Western Pacific Ocean, the Amazon basin of South America, and some parts of equatorial Africa.

Height data are taken from Ramage and Raman (1972). 8 Seasonal Migration of the Equatorial Heat Source 21 In regions where monsoon is interhemispheric, the forcing for cross-equatorial flow appears to be provided by the isallobaric gradient between the heat source on one side and the heat sink on the other. The crossing appears to open a floodgate for cold, humid airmass of the winter hemisphere to rush into the summer hemisphere to start the process of advance of summer monsoon in that hemisphere.

The wave axis, which tilts eastward with height at the eastern end of the islands, becomes vertical in the central region and acquires an opposite tilt in the west. The change in the tilt is believed to be caused by the variation with longitude of the vertical shear of the basic current, as shown in Fig. 4. 0N, 171E) which lies near the eastern end and also from that of the mean of three island stations which lie in between. Yanai (1964) suggested a model of the easterly wave based on his studies in the equatorial eastern Pacific, which is shown in Fig.

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