|
|
|
|
|
|
|
|
|
Hatchery
| Fisheries glossary |
- The process of cultivating and breeding a large number of juveniles in an enclosed environment. the juveniles are then released into lakes, rivers or fish farm enclosures.
- A facility where fish eggs are hatched and the fry raised, especially to stock lakes, streams, and ponds.
|
Инкубаторий, русский
|
Environment, английский
- Surrounding in which operates, including air, water, land, natural resources, flora, fauna, humans and their interaction.
- Окружающая среда. совокупность всех материальных тел, сил и явлений природы, ее вещество и пространство, любая деятельность человека, находящегося в непосредственном контакте с живыми организмами; совокупность абиотической, биотической и социальной сред,
- Окружающие условия [среда]; внешние факторы или воздействия; условия эксплуатации ` (лл)
- The conditions and influences under which an organism lives
- N 1 лнгв. окружение; 2 псхл. окружающая обстановка5 consonantal ~ консонантное окружение epanalepsis n эпаналепсис, удвоение6 epenthesis n 1 эпентеза, вставка звуков1; 2 добавление гласного звука для того, чтобы 3 английский как язык международного общения. 4 несовпадение стиховых и фразовых границ. 5 внешний контекст, в котором происходит наше поведение. 6 фигура речи, состоящая в повторе слова, словосочетания или пред- ложения. epenthetic 41 evaluation разбить труднопроизносимую группу (кла- стер) согласных
- Окружающая среда
- Окружающая среда; при- родно-ландшафтная среда
- The place in which an organism lives, and the circumstances under which it lives. environment includes measures like moisture and temperature, as much as it refers to the actual physical place where an organism is found.
- The combination of all the external conditions and the potential effect of the inner environment (heteromosaic of abiotic conditions). e. change: survival depends on the life span of the organisms involved, and has to adapt to a new situation via genetic change, evolution, etc. • cyclic change: rhythmically repetitive, like cycles of a season, day / night, movement of tides etc. • directional change: change is maintained over a long period in relation to the life span of organisms - erosion, siltation, cycles of glaciation, etc. • erratic change: these have no rhythm and no consistent direction e.g., hurricanes, cyclones, flash storms, fires, vulcanos, earthquake, etc.
- Окружающая среда. существующая в данный момент совокупность всех внешних условий и воздействий, которым подвержена данная система (или организм) (мос, 14). `36
- (1) the system of surrounding things, conditions or influences, especially affecting the existence or development of someone, something or another system (->habitat), (2) the art of environing, (3) the state of being environed.
- A global context in which to access data.
- A set of roles that are required to run a specific application and the machines to be used for each role.
- One of two deployment destinations within a microsoft azure cloud service: staging or production.
- The totality of surrounding conditions and circumstances affecting growth or development. often the term is applied to the natural features of a geographic area: water, air, and land — including ecological relationships.
- The sum of the physical, chemical, and biological factors that surround an organism.
Enclosures, английский
Международный конгресс по пространственным оболочечный покрытиям
Especially, английский
|
Spawning, английский
The production or depositing of large quantities of eggs in water.
Upwelling, английский
- The process by which water, usually cold and nutrient-rich, rises from a deeper to a shallower depth. this is often a result of offshore surface water flow, particularly when persistent wind blows parallel to a coastland and the resultant ekman transport
- The oceans are layered; with sunwarmed water on top, and colder water containing 343 upwelling nutrients and dissolved gases below. upwelling is a phenomenon that brings this deeper water to the surface. when nutrients rise towards the sunlight, microscopic plants (phytoplankton) combine them with carbon dioxide and solar energy by photosynthesis. the organic compounds thus produced form the basis of the oceanic food chain. oceanographers have identified many different forms of this phenomenon, the more significant of which are: • coastal upwelling: coriolis effect causes winddriven currents to move to the right of winds in the northern hemisphere. thus winds blowing south along an eastern land-ocean boundary, or north along a western one, drive surface water away from the coast, allowing cold, nutrient-rich deep water to rise and replace it. in the southern hemisphere, these directions are reversed. some of the world’s most productive fishing grounds are in regions where coastal upwelling occurs. • equatorial upwelling: a related phenomenon. the equatorial surface current flows from east to west in both the atlantic and pacific basins. coriolis force turns the flow away from the equator (north to the right, south to the left) once again clearing a path for colder water to rise from the depths. as phytoplankton feast on the rising nutrients they bloom, causing the water to become green and murky—to the extent that space travelers can visually locate the pacific equatorial region by a line of high phytoplankton concentration. • dynamic uplift: occurs in response to variations in coastal ocean currents and is independent of coastal wind conditions. • tidal pumping: strong tidal currents produce upwelling through amplification and associated topographic turbulence. during flood tide, oceanic water mixes with and transfers part of its nutrient load to the shelf water before being removed again during ebb tide. each flood tide brings another load of nutrients, and the resulting enrichment can be substantial. marine life on the great barrier reef benefits greatly from tidal pumping, as do similar geographical settings where tidal currents are amplified in channels between islands. • eddy formation:western boundary currents spawn several eddies per year, each of which maintains its identity for two years or longer. warm core eddies are characterized by a deep thermocline in the centre and shallow thermocline around the eddy fringe. as they impinge on the continental slope, the thermocline is lifted up, having the same effect as when the main current impinges on the shelf.
- The raising of benthic nutrients to the surface waters. this occurs in regions where the flow of water brings currents of differing temperatures together, and increases productivity of the ecosystem.
- A rising of nutrient-rich water toward the sea surface.
|
|
|
|
|
|
|
