Категория:Моделирование рельефа

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Следствия:

Желания и лица - как отобразить - Переворот по Джанибекову

aw:Category:Geodata

lw:Category:Earth

goals[edit]

Интересно, если бы кто-то разбирающийся с ясным разумом сделал геологическую реконструкцию с картами, картинками, обоснованиями.

solutions[edit]

The calculation of variations in the sea level is relatively simple. It is by far more complicated to then determine the change in the water mass. A team of geodesists and oceanographers from the University of Bonn, as well as from the GFZ German Research Centre for Geosciences and the Alfred-Wegener Institute for Polar and Marine Sciences, two centres of the Helmholtz Association, have now, for the first time succeeded in doing this. The researchers were able to observe short-term fluctuations in the spatial distribution of the ocean water masses.

we were able to prove, for the first time, that in particular in the higher latitudes, significant fluctuations of the water mass occur, and that this takes place within a time period of only one to two weeks". So far one only knew that the mass of the world-wide ocean water varies seasonally by on average approximately three quadrillion kilogrammes (a quadrillion equals to 1 followed by 15 zeroes) -- that implies a sea level variation of approx. seven to eight millimetres. This effect is brought about, among others, by variations in precipitation and evaporation as well as by the storage of water as snow. But, also, the melting of the glaciers and the ice masses in Greenland and in the Antarctic play a role.

Subcategories

This category has the following 3 subcategories, out of 3 total.

З

► Законы изменения рельефа Земли‎ (5 P)

М

► Модель рельефа Земли‎ (7 C, 10 P)

Э

► Эмпирические данные про рельеф Земли‎ (1 P)

Pages in category "Моделирование рельефа"

The following 3 pages are in this category, out of 3 total.

R

Шаблон:Relief

В

Вносить в mediawiki карты, границы, пути

Г

Геострофия

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