卡塔尔专属经济区物理和生物地球化学参数的变异

A. Mohammed, Fazle Rakib, I. S. Al-Ansari, Y. S. Hûsrevoğlu, O. Yigiterhan, I. Al-maslamani, Vethamony Ponnumony
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引用次数: 0

摘要

对卡塔尔专属经济区(EEZ)夏季末(2014年9月)和冬季(2015年1月)沿样带收集的海洋学数据进行了分析,探讨了水文和生物地球化学的时空变化。研究表明,9月份深水区以分层为主,从表面到底部的垂直变化约为9°C。然而,由于强风混合和地面冷却,1月份水柱保持均匀性。两个季节,专属经济区上层溶解氧(DO)均处于合理范围,而1月份,中下层溶解氧随深度逐渐减少。这会导致夏季缺氧。夏季,近海地区叶绿素-a (Chl-a)相对较高,而近岸地区则很低。物理和生物地球化学参数的变化对卡塔尔专属经济区的初级生产力有显著影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Variability of Physical and Biogeochemical Parameters in the Exclusive Economic Zone of Qatar
The oceanographic data collected along a transect in the Exclusive Economic Zone (EEZ) of Qatar during late summer (September 2014) and winter (January 2015) have been analyzed to investigate the spatial and temporal variability of hydrography and biogeochemistry. The study reveals that stratification is dominant in the deep-water regions during September, with a vertical variation of around 9 °C from surface to bottom. However, the water column remains in homogeneity during January due to strong wind mixing and surface cooling. The dissolved oxygen (DO) in the upper layer of the EEZ is on a reasonable range in both the seasons, while they gradually decrease with respect to depth in the mid and bottom layers during January. This leads to hypoxic conditions in summer. Chlorophyll-a (Chl-a ) is relatively high during summer in the offshore region, while that in the nearshore regions is very low. The variability in the physical and biogeochemical parameters has shown significant effects in primary productivity in the EEZ of Qatar.
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