Li Yizhen, He Ruoying, McGillicuddy Dennis J, Anderson Donald M, Keafer Bruce A
Department of Maine, Earth and Atmospheric Sciences, North Carolina State University.
Department of Applied Ocean Physics and Engineering, Woods Hole Oceanographic Institution.
Cont Shelf Res. 2009 Sep 30;29(17):2069-2082. doi: 10.1016/j.csr.2009.07.012. Epub 2009 Aug 5.
In situ observations and a coupled bio-physical model were used to study the germination, initiation, and development of the Gulf of Maine (GOM) bloom in 2006. Hydrographic measurements and comparisons with GOM climatology indicate that 2006 was a year with normal coastal water temperature, salinity, current and river runoff conditions. cyst abundance in bottom sediments preceding the 2006 bloom was at a moderate level compared to other recent annual cyst survey data. We used the coupled bio-physical model to hindcast coastal circulation and cell concentrations. Field data including water temperature, salinity, velocity time series and surface cell concentration maps were applied to gauge the model's fidelity. The coupled model is capable of reproducing the hydrodynamics and the temporal and spatial distributions of cell concentration reasonably well. Model hindcast solutions were further used to diagnose physical and biological factors controlling the bloom dynamics. Surface wind fields modulated the bloom's horizontal and vertical distribution. The initial cyst distribution was found to be the dominant factor affecting the severity and the interannual variability of the bloom. Initial cyst abundance for the 2006 bloom was about 50% of that prior to the 2005 bloom. As the result, the time-averaged gulf-wide cell concentration in 2006 was also only about 60% of that in 2005. In addition, weaker alongshore currents and episodic upwelling-favorable winds in 2006 reduced the spatial extent of the bloom as compared with 2005.
利用现场观测和一个生物物理耦合模型,研究了2006年缅因湾(GOM)水华的萌发、起始和发展情况。水文测量以及与GOM气候学的比较表明,2006年是沿海水温、盐度、海流和河流径流条件正常的一年。与其他近期年度孢囊调查数据相比,2006年水华之前底部沉积物中的孢囊丰度处于中等水平。我们使用生物物理耦合模型来后推沿岸环流和细胞浓度。包括水温、盐度、流速时间序列和表层细胞浓度图在内的现场数据被用于评估模型的逼真度。耦合模型能够较好地再现水动力以及细胞浓度的时空分布。模型后推解进一步用于诊断控制水华动态的物理和生物因素。表层风场调节了水华的水平和垂直分布。发现初始孢囊分布是影响水华严重程度和年际变化的主导因素。2006年水华的初始孢囊丰度约为2005年水华之前的50%。因此,2006年整个海湾的时间平均细胞浓度也仅约为2005年的60%。此外,与2005年相比,2006年较弱的沿岸海流和间歇性的有利于上升流的风减少了水华的空间范围。