Abstract

Abstract Wind data from the European Remote-Sensing Satellite (ERS-1) scatterometer are used to depict wind fields in coastal waters around New Zealand. They include mesoscale detail not resolved by present operational models nor from general ships' data due to the low density of observations. These wind data reveal regions of local wind intensification (low-level jet) associated with the ends of orographic barriers. New Zealand has steep and high orography, which frequently induces orographic lee troughs. The jets are particularly evident streaming over coastal waters beyond the ends of these lee troughs. Using a year of scatterometer data, these jets are identified and characterized. Some necessary conditions for their occurrence are established, namely, the general direction of the flow in relation to orographic features, the threshold stability of the airstream, and the degree of orographic blocking. The formation of these jets requires the Brunt-Vaisala frequency for the lower atmosphere, up to a hei...

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