长期的生产变化

I. Marasović, B. Grbec, M. Morović
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引用次数: 28

摘要

在亚得里亚海中部观察到初级生产力的长期波动和趋势。生产率的变化是由长期影响亚得里亚海地中海水域平流的海洋和气象因素造成的。特别注意1978年开始的初级生产的突然和长期增长。这一增长与地中海水域(营养丰富)向亚得里亚海的平流增强有关。地中海水域向亚得里亚海的平流增加可归因于全球气候变化。
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Long-term production changes in the adriatic

Long-term fluctuations and trends in the rate of primary production were observed in the middle Adriatic Sea. Variability in the production rate was caused by oceanographic and meteorological factors affecting the advection of the Mediterranean waters in the Adriatic on long-term scale.

Particular attention is given to a sudden and prolonged increase in primary production that started in 1978. This increase is related to the enhanced advection of the Mediterranean waters (richer in nutrients) into the Adriatic. Increased advection of Mediterranean waters to the Adriatic can be attributed to global climatic changes.

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