Longitudinal Differences of Phytoplankton Community during a Period of Small Water Level Fluctuations in a Subtropical Reservoir Bay (Xiangxi Bay,Three Gorges Reservoir,China)

The Three Gorges Reservoir (TGR) had a great inflow discharge with small water level fluctuations in the flood season of the year 2008, when a large‐scale cyanobacterial bloom broke out in Xiangxi Bay (a tributary bay behaving like a lake) for the first time after the construction of the TGR impoundment. To compare spatiotemporal longitudinal differences of phytoplankton community structure during this period, weekly surveys were performed in Xiangxi Bay. The cyanobacterial bloom lasted from June 6 to July 18, 2008, with Microcystis aeruginosa as the dominant species. During this bloom the species diversity, evenness and community change rate was relatively low. The probable causes for the interruption of the bloom were precipitation and water temperature. In the non‐cyanobacterial bloom period (July 25 to September 26, 2008) many other species dominated the community including Stephanodiscus hantzschii and Cryptomonas ovata, with higher values of species diversity, evenness and community change rate. As for the longitudinal differences, the community structure in the riverine zone was different from that in other zones, indicating the important effect of inflow from the upstream of Xiangxi Bay. The management actions in Xiangxi Bay should prevent blooms in the mainstream, lacustrine and transitional zone. (© 2011 WILEY‐VCH Verlag GmbH & Co. KGaA, Weinheim)     

River–reservoir transition zones are nitrogen fixation hot spots regardless of ecosystem trophic state

Reservoir hydrodynamics may create heterogeneity in nitrogen (N) fixation along the riverine–transition–lacustrine gradient. In particular, N fixation may be highest in reservoir transition zones where phytoplankton biomass is also expected to be relatively high. We investigated spatial patterns of N fixation in three Texas (USA) reservoirs of varying trophic state. We sampled 6–9 stations along the longitudinal axes of the major inflows and measured N fixation using the acetylene reduction method. Total N, total phosphorus (P), and algal biomass (as chlorophyll-a) were also measured at each sample location. Measurable N fixation was observed in all reservoirs and was light-dependent. Nitrogen fixation was consistently low in the riverine zone, highest in the transition zone, and low in lacustrine zone of all reservoirs. The absolute magnitude of N fixation was similar in two relatively unproductive reservoirs and an order of magnitude higher in the eutrophic reservoir. A similar pattern was observed in mean nutrient and chlorophyll-a concentrations among reservoirs. However, chlorophyll-a concentrations were highest in the riverine zone of each reservoir and exhibited a monotonic decrease in the downstream direction. Maximum chlorophyll-a concentrations did not coincide with maximum N fixation rates. Results of our study indicate that reservoir transition zones can be biogeochemical hot spots for planktonic N fixation, regardless of trophic state. Therefore, transition zones may be the most at risk locations for water quality degradation associated with increased reservoir productivity. Water quality managers and aquatic scientists should consider the spatial heterogeneity imposed by unique hydrodynamic controls in reservoir ecosystems. Handling editor: Luigi Naselli-Flores     

在不同蓄水位下三峡库区春季水华特征及趋势分析

基于2004—2015年三峡库区支流春季水华的监测数据,开展了三峡库区不同蓄水位下春季水华特征及趋势分析。结果表明:总共有26条支流发生春季水华,香溪河为水华发生概率最高的支流。水华藻类优势种主要是硅藻和甲藻,甲藻水华出现的概率随着蓄水位的增加而增加,但是在持续几年175 m蓄水之后,甲藻水华出现的频率下降,硅藻水华出现的频率增加。在175 m蓄水之前,水华发生期藻类密度、叶绿素a含量及水体营养盐水平相对较低,此后都有了较高的提升,但是在持续几年175 m蓄水之后,藻类密度、叶绿素a浓度以及营养盐浓度都有下降趋势。对藻密度及叶绿素a含量与主要环境因子进行主成分分析(Principal components analysis)发现,藻密度和叶绿素a与总磷、总氮、高锰酸盐指数聚类一簇,藻密度、叶绿素a浓度与总磷、溶解氧、高锰酸盐指数显著正相关。在蓄水之后,三峡库区支流营养水平有所增加,随着蓄水位的增加,三峡库区支流断面的平均流速降低,在合适的温度下,三峡库区支流水华易发生。     

Immediate impacts of the second impoundment on fish communities in the Three Gorges Reservoir

Long and short term investigations have revealed dramatic changes in fish communities after impoundments by reservoirs. However, the process of these changes during impoundment remains poorly studied. In 2005 and 2006, before and during the second stage of impoundment of the Three Gorges Reservoir (TGR), in the upper reaches of the Yangtze, China, we investigated fish catches to assess the impacts of reservoir filling on fish community structure. We conducted sampling at 2 sites, Wanzhou reach, which had been inundated by the first water filling in 2003, and Fuling reach, which still remained a riverine site before this water filling. The results revealed an evident and immediate shift of fish communities from lotic to lentic components. In the Wanzhou reach, during the filling, the abundance percentage of lentic fish increased to 94% compared to 69% before the filling. In the Fuling reach, after the filling, lotic fish declined in abundance from 99% to 85%, while lentic fish increased from less than 1% to 12% in abundance. Based on our investigation and the regulation scheme of the TGR, we predicted that after the completion of the Three Gorges Dam (TGD), there would be typical lacustrine, transitional and riverine zones in TGR, with their corresponding fish assemblages. We suggest that long term monitoring should be conducted to evaluate the future ecological effects, and different strategies implemented in these three zones for conservation purposes.     

汤溪水库富营养化特征与水质管理对策

通过2003年对广东省汤溪水库水生态学进行调查,分析了该水库的富营养化特征,并从流域管理和水动力学两个方面对水库水质管理对策进行了探讨。汤溪水库为中度富营养化水体,具有明显时空分布差异,丰水期富营养程度高于枯水期,溪头河流区高于新桥河流区。蓝藻是水库浮游植物的主要优势类群,其中引发水华的铜绿微囊藻(Microcystis aeruginosa)为优势种。水库上游集水流域分布近30万居民,大量的生活排污和农业污染形成了主要的外源污染源,这些外源污染的输入是水库水体营养盐的主要来源;合理处理上游居民生活垃圾、减少生活污染中磷含量、增加流域和库区周围植被覆盖、合理使用农业化肥是降低水库表层水体中营养盐浓度的主要途径。由于该水库的蓝藻和富营养化水平直接与水体的稳定性有关,利用对水库排水的可控制性调节水库水体的稳定性,可作为控制蓝藻水华发生的有效途径。     

Responses of spring phytoplankton communities to their habitats in the Xiangxi Bay of Three Gorges Reservoir,China

Since the water storage was initiated in 2003, the environment of Three Gorges Reservoir (TGR) has changed significantly. Algal blooms and eutrophication have been a frequent occurrence, with serious eutrophication in the tributary bays. To provide some theoretical evidence for the prevention and control of algal blooms, the goal of this study is to elucidate factors that influence algal blooms at different sections of the Xiangxi Bay (XXB). Using field data from the XXB, the responses of phytoplankton communities to their habitats were investigated from March to May, 2010. The results indicated a significant spatial and temporal heterogeneity in phytoplankton composition, cellular abundance, and habitats in the spring. Fifty-four genera representing 6 phyla were monitored. Redundancy analysis indicated that the variation in water temperature and relative water column stability (RWCS) contributed greatly to the succession of spring phytoplankton. Due to different physiological adaptabilities and mechanisms of competition among the algae species, significant succession of the community structure had been observed. The predominant species appears to have changed from those adapted to low temperatures and strong mixing (dinoflagellates and diatoms) to those adapted to high temperatures and weak mixing (green algae and cyanobacteria). The lack of silicate resulted in the succession from diatoms to green algae. Due to the influence of the Yangtze River, there is a low potential for algal blooms at lower reaches of the bay because of frequent water exchange. In contrast, the potential is high at middle and upper reaches where the water temperature increases gradually. The hierarchical status of the two sections is significantly different. Precipitation would inhibit algal blooms somewhat, and heavy rainfall would eliminate algal blooms throughout the bay. Phytoplankton are sensitive to their changing habitat in XXB. For a bloom to occur, sufficient nutrients, a lower flow velocity, and appropriate temperature and light conditions are necessary. As an artificial regulating reservoir, proper ecological regulation could not only significantly affect the dynamic conditions of the water body tributaries, but it could also change the transfer characteristics of light and heat, abolishing the algae habitats and thereby inhibiting the water bloom.     

三峡水库富营养化问题与对策研究

三峡水库蓄水后,大部分库湾已出现富营养化态势,并暴发了数次以甲藻(拟多甲藻)和硅藻(小环藻)为主的水华现象,特别是在春季。以香溪河库湾为例,分析两周年的营养状态变化,总体上说,除冬季外,大多数月份为富营养,在春季则为重富营养。对三峡水库22条入库支流库湾的营养状态进行综合评价,结果表明,有5条(22.7%)支流库湾为中营养,17条(77.3%)支流库湾为富营养(重富营养化支流库湾有10条,占45.5%);但三峡水库本身水质尚好,仍保持中营养状态。统计分析表明,入库支流流域的年均流量和流域面积与支流库湾叶绿素a存在显著负相关关系,说明支流库湾越小或年均流量越小,藻类叶绿素a浓度就越高,即越容易在春季形成水华。文中讨论了控制和减缓富营养化几项措施。       

Modeling the effects of the streamflow changes of Xinjiang Basin in future climate scenarios on the hydrodynamic conditions in Lake Poyang,China

The responses of lake hydrodynamics to the hydrological processes in watersheds have been associated with the ecological evolution of and the biochemical processes in aquatic ecosystems. This paper investigates how the changes in the streamflow of Xinjiang Basin in different future climate scenarios could affect the hydrodynamic conditions in Lake Poyang. First, the hydrodynamic processes in Lake Poyang (i.e., lake level and water velocity) were simulated based on the environmental fluid dynamics code (EFDC). Error statistics indicated that the hydrodynamic model reasonably reflected the hydrodynamics in Lake Poyang. Second, the future streamflow of Xinjiang Basin from 2016 to 2050, which was projected in two future climate scenarios (Sim_RCP4.5 and Sim_RCP8.5) based on the Xin’anjiang model, was applied to hydrodynamic modeling to investigate the relationship between future discharge and hydrodynamics. Results showed that the streamflow changes of Xinjiang Basin in future climate scenarios considerably affected the seasonal distribution of the flow field in Lake Poyang. The hydrodynamic change region that exceeded the threshold values under these two climate scenarios both demonstrated a fluctuating trend and nearly covered the entire lake until April. In Sim_RCP8.5 a slightly larger area was influenced than in Sim_RCP4.5, except in January, and the eastern channel was always significantly affected by streamflow change. These analyses can enhance the present understanding of the relationships between the hydrodynamics in lakes and the hydrological processes of sub-basins.     

Experimentation,modelling, and simulation of hydrochory in an Amazonian river

1. Seed transport by hydrochory is a key mechanism of long-distance dispersal constrained by attributes of the seed and hydrodynamics of the river, influenced by seasonal precipitation and hydrological pulses. However, the extent to which a hydrodynamic model can predict seed dispersal influenced by a tributary is unknown.
2. The study was conducted along a 10-km stretch of the Falsino River in Amapá, Brazil. Hydrodynamic parameters from the 2021 rainy season were used to calibrate a three-dimensional numerical model (SisBaHia) and simulate hydrochory of Macrolobium bifolium, a widely distributed species in the Amazon floodplains. This model was coupled with a Lagrangian dispersal model to estimate the average transport distance of the fruit plume. The simulated results were compared statistically with those of dispersal quantified in the field.
3. The field experiment coincided with the maximum hydrological pulse, providing with a maximum potential distance of longitudinal dispersal fruit of c. 10 km in 2 hr. The orders of magnitude of the mean plume transport (observed and numerically simulated centre of mass) were compatible with each other over six longitudinal tracking sections (4.0% ≤ estimated × observed error ≤ 16.5%). Different channel stretches had distinct hydraulic characteristics that influenced spatial dispersal dynamics and are likely to be factors influencing the distribution of M. bifolium in these environments.
4. The present research is a contribution to understanding fluvial hydrodynamics and hydrochory by M. bifolium, whose seed dispersal syndrome is an adaptive characteristic that might explain its abundance and richness in these Amazonian riparian zones. We used M. bifolium as a model species to understand the role of seasonal flood pulse and fluvial hydrodynamics related to hydrochory favouring.

     

The Importance of Hydrodynamics for Protected and Endangered Biodiversity of Lowland Rivers

This paper examines the relationship between protected and endangered riverine species (target species) and hydrodynamics in river-floodplain ecosystems, combining ecological and policy-legal aspects of biodiversity conservation in river management. The importance of different hydrodynamic conditions along a lateral gradient was quantified for various taxonomic groups. Our results show that (i) target species require ecotopes along the entire hydrodynamic gradient; (ii) different parts of the hydrodynamic gradient are important to different species, belonging to different taxonomic groups; (iii) in particular low-dynamic parts are important for many species and (iv) species differ in their specificity for hydrodynamic conditions. Many species of higher plants, fish and butterflies have a narrow range for hydrodynamics and many species of birds and mammals use ecotopes along the entire gradient. Even when focussing only on target species, the entire natural hydrodynamic gradient is important. This means that the riverine species assemblage as a whole can benefit from measures focussing on target species only. River reconstruction and management should aim at re-establishing the entire hydrodynamic gradient, increasing the spatial heterogeneity of hydrodynamic conditions.     

Temporal variations in phytoplankton, particulates, and colored dissolved organic material based on optical properties during a Long Island brown tide compared to an adjacent embayment

Since 1985, the coastal embayments of Long Island, New York, have been plagued with recurrent blooms, aptly called brown tides, of the pelagophyte Aureococcus anophagefferens. The distinct ocean color observed during these blooms suggests that optical methods can be used as a tool to study, detect, and track brown tides. Thus, the goal of our project was to compare the optical properties and pigment composition during bloom and non-bloom conditions and assess temporal variations in the phytoplankton and other constituents in the seawater associated with bloom development. From 17 May to 8 June 2000, we measured a time series of particle size distributions and concentrations as well as size-fractioned algal pigments and optical properties in two Long Island embayments where brown tides are known to occur. During our study, A. anophagefferens represented an insignificant contribution to the algal community in West Neck Bay (WNB), whereas a bloom developed in Quantuck Bay (QB). Initially, temperature and salinity were similar at the two locations; however, bulk optical properties, chlorophyll, and particle concentrations were nearly a factor of 2 greater at QB. Bulk optical properties remained constant at WNB, yet increased exponentially at QB as the bloom developed. The composition of particulates, including phytoplankton, varied little at QB, and the optical properties suggested the dominance of A. anophagefferens (confirmed by microscopy). The largest temporal variations were observed in the colored dissolved organic material (CDOM); the colloidal (0.2–0.7 μm) fraction, exhibiting a strong protein-like signal, increased dramatically at the height of the bloom. At WNB particle sizes and algal composition varied despite the invariant bulk optical properties; CDOM variations were minimal. Overall, the optical properties in the two bays demonstrated that at QB temporal variations were dominated by biomass and colloidal protein changes, whereas shifts in the algal community occurred at WNB. This study demonstrates the utility of in situ optical observations to resolve temporal changes in the ecological conditions associated with algal bloom development.     

Hydrodynamic control of filamentous macroalgae in a sub-tropical spring-fed river in Florida,USA

Hydrodynamic properties of rivers and streams are primary controls on the abundance and structure of algal communities. In Florida, USA, filamentous macroalgal proliferation in spring-fed rivers has largely been attributed to nitrogen enrichment; however, changes in hydrodynamics and other potential mechanisms have not been thoroughly evaluated. This study tested whether macroalgal abundance (primarily Lyngbya wollei) was related to hydrodynamics in Gum Slough, a sub-tropical Florida spring-fed river. Flow velocities and macroalgal cover were measured at three transects bimonthly between June 2010 and January 2013, a period during which river discharge fluctuated in response to a drought and a tropical storm. Temporal variation in macroalgal cover was significantly inversely related to flow velocity, excluding fall/winter sampling events when light limitation was likely. The results indicate a velocity threshold below which macroalgal cover increased substantially, and a lower threshold below which complete cover frequently occurred. Local differences in channel morphology and substrate type (i.e., aquatic plant beds) seemed to affect the relationship between macroalgal cover and velocity at each transect. Nitrogen and phosphorus concentrations and other water chemistry parameters were not associated with variation in macroalgal cover. Overall, this study suggests that hydrodynamics can strongly control filamentous macroalgae in Florida spring-fed rivers.     

流溪河水库丰水年与枯水年营养盐动态的比较分析

流溪河水库是一座位于北回归线上的大型山谷型水库,典型的热带-亚热带过渡区水体。为了解该水库的营养盐动态特征,于2008-2009年对水库的营养盐状况和环境因子进行了逐月监测,分析了其丰水年(2008)和枯水年(2009)营养盐动态的动态特征和影响因素。两年的降雨量分别为2660mm和1583mm,降雨主要集中在季风期(4-9月)。丰水期初期(4-5月)是全年营养盐浓度最高的时期,该时期丰水年与枯水年的营养盐空间分布相似:营养盐浓度沿入库河流至水库大坝方向递减,地表径流带来的外源输入是这个期间营养盐变化的主要因素。河流区的营养盐主要受地表径流带来的外源输入的影响,湖泊区营养盐主要受水位变化导致的内源输入的影响。较大的降雨量差异导致两年不同的营养盐季节动态,丰水年有着更高的营养盐水平,更小的DIN/TN与DIP/TP值。河流区较高的营养盐水平会带来湖泊区较高的TN浓度,但不会导致湖泊区更高的TP浓度。     

澜沧江梯级开发下鱼类支流生境替代效果

作为干流高坝水电开发导致鱼类生境丧失的一种补偿措施，支流替代生境近年来被广泛应用于受工程影响河段的土著鱼类保护，但替代支流发挥怎样的保护效果及干流对其的影响仍不清楚。以实施了澜沧江梯级生境替代的支流基独河与罗梭江为研究对象，并选择了邻近的对照支流，通过对鱼类调查数据的分析对比，揭示了各支流鱼类种类组成与群落结构的差异特征，初步阐明了梯级开发下鱼类支流生境替代效果以及干流工程建设对其的影响。结果表明：澜沧江支流替代生境对干流鱼类具有明显的保护作用，支流生境修复后鱼类物种丰富度明显提高，罗梭江土著鱼类、特有鱼类物种数分别增加了12种、7种，基独河则是7种、2种，替代生境能为澜沧江土著鱼类、部分濒危特有鱼类和洄游鱼类提供完成生活史的关键栖息地。干流对支流生境替代保护有着重要影响，罗梭江、基独河与邻近干流鱼类群落的Bray-Curtis相似性分别为21.76%、10.73%,支流河口段保持“河相”是支流生境替代保护效果可持续的关键。综合考虑生境替代保护的效益与投入，建议今后开展此类保护措施时优先选择库尾河相区的支流。     

三峡水库生态渔业发展策略与关键技术研究分析

针对三峡水库蓄水后水体资源丰富、水生态系统发育尚不完善、支流库湾藻类水华问题较严重、鱼类群落结构有待调控、水生生物资源未有效利用和转化的现状, 阐述了三峡水库生态渔业作为生态系统保护途径和绿色产业的必要性与重要性, 提出了三峡水库生态渔业发展的总体目标与基本原则, 认为三峡水库发展生态渔业应以生态安全保障和水质养护为首要任务, 严格控制外来物种的引种移植, 以土著鱼类自然繁殖保护和捕捞管理为主, 动态调控放流增殖的鱼类种类和数量为辅, 建立以鱼类群落合理配置和食物网结构优化为手段的水库生态系统调控技术体系, 促进高效的物质循环和能量流动, 实现环境保护和渔业增效的双赢。作者围绕渔业放流增殖、野生鱼类资源保护、捕捞管理、局部库区渔业调控、渔业生物控藻、社区渔业协调管理、生态渔业总体规划等方面, 分析了现阶段三峡水库生态渔业的重点研究任务与关键技术,同时建议加强相关生态学理论与方法研究、技术示范和成果应用, 为三峡水库以渔养水、渔-水和谐的综合管理提供决策依据。       

Spatial Distribution of Macroinvertebrate Community along a Longitudinal Gradient in a Eutrophic Reservoir‐Bay during Different Impoundment Stages,China

The longitudinal patterns of the macroinvertebrate community in the Xiangxi Bay of the Three Gorges Reservoir (TGR) were investigated during the second (2nd) and third (3rd) impoundment stages (October 2006–July 2010), to test the effects of increased water level fluctuations (WLF) on the macroinvertebrates. By comparing to the former reports of the first (1st) impoundment stage (inter‐annual WLF 4 m), we found that oligochaetes dominated in three different stages in the Xiangxi Bay. However, the total abundance of macroinvertebrates showed a dramatical decline from the 1st to 2nd stage (inter‐annual WLF 11 m), but changed slightly from the 2nd to 3rd stage (inter‐annual WLF 30 m). This indicated that higher WLF in the 2nd stage had already greatly reduced the macroinvertebrates abundance, thereby the disturbance in the 3rd stage could only slightly affect the already reduced abundance. Three longitudinal zones (the mainstream zone, the lacustrine zone and the transitional zone) were found based on the macroinvertebrate density, biomass, and taxa richness, combined with the geographical location of each site. Significant differences in density and biomass of macroinvertebrate were found among different zones (P < 0.05), yet no significant difference was found in taxa richness (P > 0.05). Two‐way indicator species analysis showed that the community type in most sites varied in different seasons from the 2nd stage, exhibiting a dynamic zonation pattern, which differed with the stable pattern of the 1st stage. This seasonal feature was coupled to the seasonal changes of the WLF. (© 2012 WILEY‐VCH Verlag GmbH & Co. KGaA, Weinheim)     

三峡水库坝前水域浮游植物群落时空动态研究

于20122013 年对三峡水库坝前水域浮游植物组成、优势种、密度、生物量及多样性进行了周年季度调查, 共鉴定浮游植物151 种属, 其中绿藻门71 种, 硅藻门47 种, 蓝藻门20 种, 隐藻门和甲藻门各4 种,裸藻门和金藻门各2 种, 黄藻门1 种。浮游植物优势种的季节更替明显, 夏季和秋季优势种类为硅藻和绿藻,冬季为硅藻、蓝藻和绿藻, 春季为绿藻、硅藻和隐藻。浮游植物年均密度和生物量分别为3.95106 ind./L 和4.078 mg/L, 空间差异表现为支流和库湾远高于干流, 季节动态表现为夏季最高, 春季和冬季次之, 秋季最低。三峡水库坝前水域浮游植物多样性指数偏低, 水体污染类型属于-中污染。研究为客观了解三峡水库坝前水域浮游植物群落的空间分布与季节变化特征提供一定的参考依据。       

Post‐Impoundment Biomass and Composition of Phytoplankton in the Yangtze River

Damming, and thus alteration of stream flow, promotes higher phytoplankton populations and encourages algal blooms (density >10⁶ cells L^–1) in the Three Gorges Reservoir (TGR). Phytoplankton composition and biomass were studied in the Yangtze River from March 2004 to May 2005. 107 taxa were identified. Diatoms were the dominant group, followed by Chlorophyta and Cyanobacteria. In the Yangtze River, algal abundance varied from 3.13 × 10³ to 3.83 × 10⁶ cells L^–1, and algal biomass was in the range of 0.06 to 659 mg C m^–3. Levels of nitrogen, phosphorus and silica did not show consistent longitudinal changes along the river and were not correlated with phytoplankton parameters. Phytoplankton abundance was negatively correlated with main channel discharge (Spearman r = –1.000, P < 0.01). Phytoplankton abundance and biomass in the Yangtze River are mainly determined by the hydrological conditions rather than by nutrient concentrations. (© 2007 WILEY‐VCH Verlag GmbH & Co. KGaA, Weinheim)     

2002-2018年滇池外海蓝藻水华暴发时空变化特征及其驱动因子

为弄清滇池外海蓝藻水华暴发时空变化规律及其影响因素,将滇池外海分为北、中、南3个区域,基于2002—2018年期间中分辨率成像光谱仪(MODIS)反演的水华面积,分析了上述3个区域蓝藻水华的时空变化特征。基于2007—2018年水文、气象和出入流数据,构建了外海三维水动力生态模型(AEM3D),并计算了各区域的水力滞留时间。通过冗余分析(RDA)、随机森林(RF)和斯皮尔曼相关分析方法,分析了影响以上区域蓝藻水华暴发的主要驱动因子。结果表明：2002—2018年期间,整个滇池外海区域年平均水华面积比(水华面积占该区域总面积比例)呈缓慢下降趋势,空间上由北向南依次递减,整个外海水华暴发面积最大主要发生在秋季。在外海北部区域,其东部水华较西部更为严重,而在中部和南部区域,呈现西部水华较东部更为严重的空间分布模式。通过对各影响因子的统计分析发现,风速、水温和日照时长是上述各区域中蓝藻水华暴发的主要决定性因素。水华暴发期间以西南风为主导风向,且上述区域的水华面积比随风速增加呈下降趋势。在外海各区域,水力滞留时间与水华暴发面积均呈显著正相关,空间上水力滞留时间由北向南逐渐增大,风速和风向是影响蓝...