Anchor ice: различия между версиями

Материал из HydroWiki
Перейти к навигации Перейти к поиску
Строка 8: Строка 8:
  
 
==Пример использования термина на английском языке==
 
==Пример использования термина на английском языке==
Frazil and '''anchor ice''' have been studied for over a century, initially inspired by severe ice-related flooding events in rivers. However, many aspects of ice accumulation in water intakes, as well as the formation of frazil and anchor ice in general, have been still unclear.<ref>Makkonen L., Tikanmäki M. Modelling frazil and anchor ice on submerged objects //Cold Regions Science and Technology. – 2018. – Т. 151. – С. 64-74.</ref>
+
[[Frazil]] and '''anchor ice''' have been studied for over a century, initially inspired by severe ice-related flooding events in rivers. However, many aspects of ice accumulation in water intakes, as well as the formation of frazil and anchor ice in general, have been still unclear.<ref>Makkonen L., Tikanmäki M. Modelling frazil and anchor ice on submerged objects //Cold Regions Science and Technology. – 2018. – Т. 151. – С. 64-74.</ref>
  
 
==Пример использования на русском языке==
 
==Пример использования на русском языке==

Версия 12:31, 10 февраля 2021

Фото донного льда [1]

Донный лед

Скопление внутриводного льда, которые закрепляются на дне.[2]

Определение на английском

In gravel bed rivers, where the rocks are suf-ficiently large to resist the ice buoyancy, the ice will be held (or anchored) on the bed, forming anchor ice[3]

Пример использования термина на английском языке

Frazil and anchor ice have been studied for over a century, initially inspired by severe ice-related flooding events in rivers. However, many aspects of ice accumulation in water intakes, as well as the formation of frazil and anchor ice in general, have been still unclear.[4]

Пример использования на русском языке

Шуга и донный лед изучались на протяжении века, первоначально интерес вызван сильными наводнениями на реках. Тем не менее, многие аспекты накопления льда на водосборах, а также формирование шуги и донного льда в целом, до сих пор остаются слабо изученными.

Список литературы

  1. https://fishki.net/2161197-donnyj-lyod.html
  2. Чеботарев А. И. Гидрологический словарь. - 3 изд. - Ленинград: Гидрометеоиздат, 1978.
  3. Hicks F. The wonderful world of river ice. CreateSpace Independent Publishing Platform. 2013.
  4. Makkonen L., Tikanmäki M. Modelling frazil and anchor ice on submerged objects //Cold Regions Science and Technology. – 2018. – Т. 151. – С. 64-74.