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The first wind zone, off Rhode Island and Massachusetts, is just 10 miles off the coast.
Compared to the preceding wind zone map, the new map specifies for many sites smaller wind loads.
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The proposed new map presents five wind zones with characteristic values from 22.5 to 32.5 m/s.
Northern Australia is affected by a northerly monsoon, partly because of the latitude and the seasonal migration of planetary wind zones and partly because of the summer heating of the continental interior that draws in surface winds.
In that context, lower plumes (h < 10 km) from high-latitude (>70°) eruptive events are likely to be confined close to the South Pole due to moderated wind zones encircled by the polar jet stream, while higher plumes have a higher potential for transcontinental ash dispersal.
Westerly and easterly QBO wind zones have wavelike structures versus altitude with vertical wavelengths about 20 km (e.g., Baldwin et al. 2001; Huesmann and Hitchman 2001).
Pogoreltsev et al. (2014) found the maximum variability of QBO winds at altitudes near 30 km (pressure levels 10 20 hPa) and determined the westerly and easterly wind zones at those heights.
In the year to the end of March, the Crown Estate saw two Round 3 offshore wind zones off the Scottish coast progress to planning stage and the first application submitted for a marine energy project in the Pentland Firth and Orkney Waters programme.
To eliminate asymmetries in the easterly and westerly wind zones, Pogoreltsev et al. (2014) proposed calculating of differences between monthly mean for each year and climatological (averaged over years 1992 2011) zonal wind velocities over the equator at the altitude of 30 km.
An alternative to calculating for wind pressure at a particular wind speed is to use the standard for various wind zones.
Southern Australia receives winter rains from depressions associated with the west-wind zone.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com