Diurnal variation of air temperature across the north pacific

Mid-West Growing Season Weather

“…When cold air going south runs into warm air, being denser it will push the warm air aside out of the way. In addition, the time of day that the cold air starts south is not bound by any rules, in contrast to what has been found in the air over the North Pacific [2] since and including the discovery by a Japanese scientist in the 1950s [3]. At a fixed location at sea level off Japan the expected noon maximum in air temperature was found to be split in two by a shallow minimum in a mean over three Because the instability that drives the cold dry air south is oriented north/south, the burst coming across the Canadian border will probably be nearly straight south to begin with.…”

“…years of data at two weather ships. Then weather data from a 35-day oceanographic cruise in March/April of 1976 found the same thing, but even more marked, while crossing the whole ocean along 35 N. Not on every day but enough times that the average of all measurements taken on the cruise showed the noon minimum (please seefigure 1of Ref [2]…”

Forming High Ozone Concentration in the Ambient Air of Southern Taiwan under the Effects of Western Pacific Subtropical High

“…When the WPSH is strong, it covers most region of East Asia, including the western rim of the Pacific Ocean extending from 15 ∘ N∼30 ∘ N to 120 ∘ E∼150 ∘ E. Besides, the WPSH may build either to the west of the Pacific Ocean or back from the west, while the westerly ridge moves east [5]. This kind shifting between the east and west of WPSH usually has an average period of 1∼2 weeks, which, however, can dominantly determine the weather patterns during its invasion period [6].…”