| | Diurnal pressure variation |
 | | With regard to latitude, the diurnal cycle has an amplitude around 1.16 hPa at the equator, and elsewhere it is proportional to the cube of the cosine of the latitude angle. |
 | | Numerical models and surface observations show that deep convection in the Amazon basin acts like a pump (4, 5), lifting the air and heating it (due to latent heat release by condensation) in the afternoon, and sinking and cooling it (by radiative flux divergence mainly in the lower troposphere) around dawn. |
 | | This is quite obvious along coastlines in warm climates, where the daytime heating of the PBL over land (but not over the ocean) produces a lower sea level pressure inland, and hence a pressure gradient which drives the sea breeze. |
| www-das.uwyo.edu /~geerts/cwx/notes/chap01/diurnal.html (503 words) |