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Föhn cloud over the Crackenback Range, near Jindabyne. The southeast Australian foehn is a westerly foehn wind and a rain shadow effect that usually occurs on the coastal plain of southern New South Wales, and as well as in southeastern Victoria and eastern Tasmania, on the leeward side of the Great Dividing Range.
The Cumberland Plain Woodland, also known as Cumberland Plain Bushland [1] and Western Sydney woodland, [2] is a grassy woodland community found predominantly in Western Sydney, New South Wales, Australia, that comprises an open tree canopy, a groundcover with grasses and herbs, usually with layers of shrubs and/or small trees.
No Australian weather stations situated in an arid region record less than 100 mm (3.94 in) of average annual rainfall. [4] The deserts in the interior and south lack any significant summer rains. The desert in western Australia is well explained by the little evaporation of the cold sea current of the West Australian Current , of polar origin ...
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Earlier this week, temperatures across the Midwest and the Northeast felt more like fall than late summer, as many people woke up to chilly mornings. In the coolest spots on Wednesday and Thursday ...
The Flyers Creek, a mostly–perennial river [2] that is part of the Lachlan sub-catchment of the Murrumbidgee catchment within the Murray–Darling basin, is located in the Central West region of New South Wales, Australia.
Doubtful Creek, formerly known as Doubtful River, a watercourse [1] that is part of the Murrumbidgee catchment within the Murray–Darling basin, is located in the Snowy Mountains district of New South Wales, Australia.
Map of New Westminster District, 1877. Senakw is marked "I.R." ("Indian Reserve") near False Creek. Sen̓áḵw was a seasonal village site of the Sḵwx̱wú7mesh (Squamish) people, located at the head of False Creek, an area abundant in natural resources such as cedar, salmon, and shellfish.