Dynamics of counter wind current along the south Sri Lanka coast during the Southwest Monsoon     

Wickramage  C. H.  Wang  Weiqiang  Arulananthan  K.  Jayathilake  Ruchira 《Ocean Dynamics》2021,71(11-12):1051-1067

Ocean Dynamics - Shipboard velocity profiles collected in July 2018 are used to study coastal current in the south of Sri Lanka during the summer monsoon. The observations reveal that there is a...  相似文献   

莫桑比克海峡及其邻近海区正压潮流数值模拟与能量收支分析*     

张华  温茜茜  彭世球 《热带海洋学报》2021,40(2):7-16

莫桑比克海峡及其邻近海区是全球海洋潮流和潮能耗散最强的海区之一。文章利用高分辨率通用环流模式对该海区的正压潮流进行模拟, 并对该海区潮能通量和潮能耗散特征进行分析。结果表明, 莫桑比克海峡及其邻近海区的潮波主要是半日分潮占主导地位, 全日分潮可忽略不计, M₂分潮形成1个左旋潮波系统和1个右旋潮波系统, S₂分潮形成1个左旋潮波系统。莫桑比克海峡和马达加斯加岛南部等绝大数区域的M₂和S₂半日潮流是逆时针旋转, 在马达加斯加岛顶部等局部区域是顺时针旋转, 而且在海峡通道等复杂地形处潮流流速量级较大。潮能通量矢量主要来自东边界, 大部分潮能通量沿马达加斯岛北部传入莫桑比克海峡区域, 其中经过马达加斯加岛北部和进入莫桑比克海峡的M₂ (S₂)分潮的潮能通量分别为156.86GW (40.53GW)和148.07GW (36.05GW), S₂分潮潮能通量的量级大约为M₂分潮的1/5~1/4。底摩擦耗散主要发生莫桑比克海峡和马达加斯加岛南北部, 其中莫桑比克海峡M₂ (S₂)分潮的底摩擦耗散为1.762GW (0.460GW), 占其底部总耗散的43.74% (39.72%)。  相似文献   

全球气候变化对红树林生态系统的影响、挑战与机遇     

王友绍 《热带海洋学报》2021,40(3):1-14

红树林是以红树植物为主体的常绿灌木或乔木组成的潮滩湿地木本植物群落, 具有“四高”特性(高生产力、高归还率、高分解率和高抗逆性)的典型海洋生态系统; 目前, 全球约有红树林1700万公顷, 主要分布在南北半球25℃等温线内。红树林生态系统的净初级生产力高达2000gC·m^-2·a^-1, 具有高强度的物质循环、能量流动以及丰富的生物多样性, 对热带、亚热带海洋生态系统的维持与发展起到关键作用, 并在全球变化过程中扮演着十分重要的角色。近30年来, 全球气候变化已引起了国内外学者的极大关注。红树林生态系统位于热带、亚热带海岸潮间带, 是一个脆弱的、敏感的生态系统, 也是首先受全球气候变化影响的典型海洋生态系统之一。作为全球海岸带地区应对全球气候变化最为重要的生态屏障之一, 气候变化将严重影响着全球红树林的生存和分布方式。本文将从全球变暖、海平面上升、大气中CO₂浓度的增加和极端天气4个主要方面, 揭示全球气候变化对红树林生态系统的影响与变化特征, 阐述红树林对全球变暖、海平面上升、大气中CO₂浓度增加和极端天气响应与适应的生态学机制, 并简要概述了红树林在减缓全球气候变化危害中的重要作用。全球气候变化也将为红树林的研究、保护和发展带来机遇与挑战。  相似文献   

Frequent central Pacific La Ni?a events may accelerate Arctic warming since the 1980s     

Jing Li  Lin Mu  Linhao Zhong 《海洋学报(英文版)》2021,40(11):62-69

Including significant warming trend, Arctic climate changes also exhibit strong interannual variations in various fields, which is suggested to be related to El Ni?o and Southern Oscillation (ENSO) events. Previous studies have demonstrated the different impacts on the Arctic of central Pacific (CP) and eastern Pacific (EP) ENSO events, and suggested these impacts are largely of opposite sign for ENSO warm and cold phases. Our results illustrate asymmetrical changes for the cold and warm ENSO events, especially for the La Ni?a events. Compared to the past frequent basin-wide cooling La Ni?a events, since the 1980s the cooling center for the La Ni?a event has strengthened and moved westward along with the increasing frequency for the canonical and CP La Ni?a events. Contrary to the basin-wide cooling and canonical La Ni?a events, the frequent CP La Ni?a events induce significant warming from the Beaufort Sea to Greenland via the convection center moving northward over the western Pacific. Observation analysis and numerical experiments both suggest that the changes in La Ni?a type may also accelerate Arctic warming.  相似文献   

大亚湾夏季浮游群落生产代谢特征及其影响因素*     

李尧  向晨晖  江志坚  宋星宇 《热带海洋学报》2021,40(6):83-92

2017年8月对大亚湾海域浮游群落初级生产、群落呼吸代谢及其平衡特征进行了研究, 并分析了其潜在环境影响因素以及对沿岸生态系统功能与健康的指示作用。研究结果表明, 大亚湾夏季海水表层呈自养状态, 而底层呈异养状态, 群落总初级生产力(gross primary productivity, GPP)、呼吸代谢速率(community respiration, CR)与净生产力(net commutnitiy production, NCP)在表层分别为1335.36±910.12、597.86±403.30和737.50±608.22mg C·m^-3·d^-1; 在底层分别为43.65±37.05、216.25±147.28和-160.27±137.01mg C·m^-3·d^-1。海湾整体呈自养状态, 水柱平均NCP为233.41±248.88mg C·m^-3·d^-1; 部分沿岸水域存在异养状态。1~200μm粒级浮游生物是GPP和CR的主要贡献者。相关性分析和主成分分析显示, NCP在表层受GPP和CR共同调控, 且与浮游植物生物量和营养盐正相关; 而在底层主要受CR影响, 且与盐度正相关。大亚湾夏季群落生产代谢平衡存在明显的水平和垂向变化, NCP的区域差异与潜在波动性对该海湾生态系统稳定性及健康状况有重要的指示作用。  相似文献   

潮滩冲淤扰动下外来与乡土红树植物幼苗稳定性差异     

潘炜杰  祝振昌  蔡宴朋  杨志峰 《热带海洋学报》2021,40(6):120-127

引种外来树种是我国各地在红树林修复实践中常用的措施。由于更容易在困难立林地存活, 外来树种被认为更具竞争优势。为弄清外来与乡土红树植物物种在困难立林地存活能力的差异及其原因, 本研究选取典型外来引种先锋树种拉关木(Laguncularia racemosa)与乡土先锋植物白骨壤(Avicennia marina)为研究对象, 通过控制实验探究潮滩冲淤扰动条件下幼苗稳定性差异及其形成机制。结果表明, 幼苗抗侵蚀能力与幼苗根冠比显著正相关, 泥沙淤积抑制幼苗根系生长, 而底床侵蚀则促进根系伸长。与白骨壤相比, 拉关木幼苗的主根更长, 根冠长度比更大, 更能抵抗底泥的侵蚀扰动, 且通过根系伸长以增强幼苗稳定性的能力也更强。拉关木幼苗比白骨壤更能适应潮滩冲淤扰动, 其竞争优势从幼苗阶段就已经建立。本研究结果可为红树林修复实践中树种和宜林地的选择提供参考, 亦可为评估外来红树物种入侵风险评价提供依据。  相似文献   

海带渣资源化利用及在小球藻培养中的应用研究     

王铭  彭敏琳  许瑾  梁翠谊  向文洲  李涛 《海洋与湖沼》2022,53(1):96-105

海带渣是海带加工中的固体废弃物,将其资源化利用生产高附加值产品具有重要意义.文章以海带渣为原料,糖化液的总还原糖质量浓度、单糖组成和小球藻培养效果为主要评估指标,探究不同预处理方法对海带渣酶解的影响,以及海带渣资源化利用培养微藻工艺的可行性.结果 显示:(1)粗纤维和灰分是海带渣主要组成成分;(2)常温常压稀硫酸预处理...  相似文献   

印度洋赤道潜流年际变化特征及其与印度洋偶极子的联系     

李俊灵  徐康  王卫强  谢强 《海洋与湖沼》2022,53(1):19-32

印度洋赤道潜流(equatorial undercurrent,EUC)是赤道流系的重要组成部分,对印度洋物质输运和能量交换有着重要意义.基于SODA 3.4.2海洋再分析数据,对印度洋EUC的三维空间结构和年际变化特征进行分析,并揭示其年际变率与印度洋偶极子(Indian Ocean dipole,IOD)的联系.结...  相似文献   

Ultra-depleted peridotite xenoliths in the Northern Taihang Mountains: Implications for the nature of the lithospheric mantle beneath the North China Craton     

《Gondwana Research》2017

We report the finding of peridotite xenoliths in the Early Cretaceous Longmengou olivine-bearing diabase (138 Ma) in the Northern Taihang Mountains in the central North China Craton. Based on the modal proportions of olivine, clinopyroxene, amphibole and anorthite, these peridotite xenoliths can be divided into three zones: clinopyroxene-bearing olivine zone (COZ), olivine-clinopyroxene zone (OCZ), and amphibole-bearing anorthite-clinopyroxene zone (AACZ). The core of olivine grains in clinopyroxene-bearing olivine zone have higher Mg^# (> 95), SiO₂ (41.80–42.53 wt%) and lower CaO (< 0.07 wt%), FeO (3.91–4.54 wt%) than the rim (Mg^# = 92.5–93.4, SiO₂ = 41.27–41.98 wt%, CaO = 0.20–0.34 wt%, and FeO = 7.02–8.87 wt%), suggesting that rim is reaction product. The core of olivine grains with higher Mg^# (> 95) and lower NiO content (< 0.04 wt%) in the clinopyroxene-bearing olivine zone was derived from ultra-depleted mantle subsequently altered by high Mg^# melts/magma with low Ni. Two generations of olivine grains occur in the OCZ where the first generation shows exsolution of ilmenite and magnetite rods containing up to 0.35 wt% TiO₂, and was likely derived from garnet peridotite hydrated by water. The second generation shows high Mg^# (96.2–97.1) and cataclastic texture, and was possibly formed by decomposition of the COZ. The occurrence of aluminous spinel suggests the role of melts with extremely high Al and Mg. Clinopyroxene in the AACZ shows systematic core-rim compositional variation with CaO and SiO₂ contents increasing towards the rim, and MgO and Fe₂O₃ concentrations decreasing from the core to the rim, indicating that the amphibole-bearing anorthite-clinopyroxene zone is a product of the reaction between mantle xenoliths and mafic magma. Plagioclase with high An value (92.0–99.95, average 97.79) indicates that the metasomatic melts have high Ca/Na and Al/Si ratios, possibly produced by the partial melting of ultra-depleted mantle under “wet” conditions. Combined with the data on other mantle xenoliths discovered in the NCC, our results suggest that the Mesozoic lithospheric mantle beneath the North Taihang Mountains within the central NCC is composed of ultra-depleted Archean and Paleoproterozoic peridotites and dunites modified by complex melts. We also propose that the destruction of eastern part of the NCC mainly occurred during Early Cretaceous, and that the boundary of the lithospheric destruction coincides with the Taihang Mountains.  相似文献   

Rapid wave-driven advective pore water exchange in a permeable coastal sediment     

《Journal of Sea Research》2004,51(2):93-107

In this study we present in-situ measurements of pore water flow velocities in a coastal sandy sediment (permeability=3.65×10⁻¹⁰ m²). The advective pore water flows were driven by the interaction of oscillating boundary flows with sediment wave ripples, (amplitude=7 cm, wavelength=30 to 50 cm). The measurements were carried out in the Mediterranean Sea at 50 to 70 cm water depth during a phase of very low wave energy (max. wave amplitude=10 cm). An optode technique is introduced that permits direct pore water flow measurements using a fluorescent tracer. Near the sediment surface (0.5 cm depth) pore water reached velocities exceeding 40 cm h⁻¹. Thus, advective transport exceeded transport by molecular diffusion by at least 3 orders of magnitude. Based on the pore water velocity measurements and ripple spacing, we calculate that 140 L m⁻² d⁻¹ are filtered through the sediment. Pore water visualisation experiments revealed a flow field with intrusion of water in the ripple troughs and pore water release at the ripple crests. The wave-driven water flow through the sediment, thus, was directly linked to the wave-generated sediment topography, and its spatial dimensions. These results show that surface waves cause water filtration through permeable sediments at water depths smaller than half the wavelength. We conclude that surface gravity waves constitute an important hydromechanical process that may convert large areas of the continental shelves into expansive filter systems. Surface gravity waves thereby could affect suspended particle concentration and cycling of matter in the shelf.  相似文献