From Wikipedia, the free encyclopedia
Glabretum[1] est pars aquae, glacie non tecta[2], in fluviis et maribus hiemalibus. In fluviis glabreta a velocitate fluminis vel a fonte quodam calidiore oriuntur. In maribus Arcticis et in aquis Oceani Australis circum Antarcticam glabreta a ventis catabaticis glaciem pellentibus gignuntur sive cum aqua calidior a flumine oceanico allata in superficiem elevatur.
Sunt in maribus Arcticis et Antarcticis glabreta, quae saepe apparent vel quotannis vel perpetuo glacie liberae manent. Quorum notissimum est Aqua Borealis in parte boreali sinus Baffiniani; glabretorum Antarcticorum glabretum Iacobi Weddell[3] nominari potest.
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