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Радиоэкологический отклик Черного моря на Чернобыльскую ядерную аварию в отношении долгоживущих радионуклидов 90Sr и 137Cs IBSS Repository
Егоров, В. Н.; Поликарпов, Г. Г.; Освас, И.; Стокозов, Н. А.; Гулин, С. Б.; Мирзоева, Н. Ю..
Исследованы потоки поступления 90Sr и 137Cs в Черное море после аварии на Чернобыльской АЭС, их миграции между компонентами экосистем, выполнены расчеты дозовых нагрузок на морские организмы за послеаварийный период, а также оценка и прогноз времени пребывания этих радионуклидов в водной среде. Получено, что время поступления 137Cs в Черное море превысит 35 лет, а количество 137Cs составит 1740 – 2440 ТБк, или 1.7 – 6.6 % от практически полного его поступления в окружающую среду из аварийного реактора ЧАЭС. Прогнозируемое поступление 90Sr в Черное море будет продолжаться свыше 70 лет, его количество за этот период составит 305 – 505 ТБк, или 3.7 – 38.8 % от его общего количества, инжектированного в окружающую среду после аварии на ЧАЭС. Вынос 137Cs...
Tipo: Journal Contribution Palavras-chave: Черное море; Радиоэкология; Радионуклиды; Миграция; Потоки; Дозовые нагрузки; Прогноз; Radionuclides; Migration; Outflow; Dose commitments; Prediction Migrations Outflow Prediction Prediction http://aims.fao.org/aos/agrovoc/c_29367.
Ano: 2002 URL: http://repository.ibss.org.ua/dspace/handle/99011/25
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A seasonal dipolar eddy near Ras Al Hamra (Sea of Oman) ArchiMer
L'Hegaret, Pierre; Lacour, Leo; Carton, Xavier; Roullet, Guillaume; Baraille, Remy; Correard, Stephanie.
Trajectories and hydrological data from two Argo floats indicate that warm and salty water at 200–300-m depths was ejected from the coast of Oman, near Ras al Hamra, in spring 2008, 2011, and 2012. This warm and salty water, Persian Gulf Water (PGW), once ejected from the coast, recirculated cyclonically in the western Sea of Oman, but also flowed eastward along the Iranian and Pakistani coasts. There, it was expelled seaward by mesoscale eddies as shown by other float data. Seasonal maps of salinity were computed from all available Argo floats; they showed that, in spring, PGW is present in the middle and north of the Sea of Oman, contrary to fall, when the salinity maxima lie southeast of Ras al Hadd. The ejection of PGW from Ras al Hamra is related here...
Tipo: Text Palavras-chave: Sea of Oman; Outflow; Eddies; Argo floats.
Ano: 2013 URL: http://archimer.ifremer.fr/doc/00171/28206/33894.pdf
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Dynamique de bord ouest en mer d'Arabie ArchiMer
Vic, Clement.
This PhD aims to investigate some western boundary processes in the Arabian Sea : (i) the life cycle of the socalled Great Whirl, a persistent mesoscale eddy; (ii) the dynamics of the Persian Gulf outflow, a marginal sea dense outflow; and (iii) the seasonal Oman upwelling, a coastal upwelling forced by summermonsoonal winds. The cornerstone of all these phenomena is their locationat a western boundary, which makes then being influenced by both localforcing (e.g., monsoonal winds) and remote forcing (Rossby waves and wesward drifting eddies). Specifically, the later are expected to impact the western boundary dynamics since the low latitude of the Arabian Sea implies a fast westward propagation of long Rossby waves and eddies. Moreover, waves are...
Tipo: Text Palavras-chave: Mer d'Arabie; Outfow; Golfe d'Oman; Golfe Persique; Ondes de Rossby; Upwelling; Dynamique de mésoéchelle et sous-mésoéchelle; Modélisation réaliste; Interactions tourbillon-topographie; Ocean modelling; Mesoscale and submesoscale dynamics; Arabian Sea; Great Whirl; Outflow; Gulf of Oman; Persian Gulf; Rossby waves; Eddy-topography interactions.
Ano: 2015 URL: https://archimer.ifremer.fr/doc/00498/60934/64328.pdf
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