“纳沙”台风引起北部湾沿岸风暴射流及其机制     

韦聪  鲍献文  丁扬  陈波 《中国海洋大学学报(自然科学版)》2022,52(3):28-39

基于FVCOM模式建立一个三维数值模型,对2011年“纳沙”台风登陆北部湾前后水位与流场变化进行了分析,并探究了风暴射流的生成机制。结果表明,广西近岸风暴射流的产生是对台风到来造成的水位起伏变化的一种正压响应;台风进入到北部湾期间,造成北部湾近岸水位先降低后升高,所导致的水位梯度差产生了驱动力,促使海水向西运动增强,从而导致在广西近海风暴射流的产生;台风登陆期间琼州海峡西向流流量增大到0.4 Sv以上,最大可达0.7 Sv;台风进入到北部湾后,促使琼州海峡西向流更多进入到北部湾,造成湾内正位涡输入增大,产生了气旋式环流来维持位涡平衡,同时气旋式环流也有利于向西运动的风暴射流增强;流经广西沿岸的风暴射流引起向西的水体输运可达0.2 Sv,对北部湾内营养盐以及污染物运移将产生重要影响。  相似文献   

论南海海洋治理——基于墨家哲学在新型国际关系上的嵌入     

余吉安  薛芮 《热带地理》2022,42(7):1190-1200

立足于中国哲学与地缘政治相融合的视角,通过解构地缘政治视角下的南海海洋治理问题,对比分析百家争鸣中墨家哲学对南海治理的价值作用,针对南海海洋治理提取墨家哲学的理念要点,尝试构建墨家哲学在南海海洋治理上的实践指导体系,研究表明：1）域内治理目标的不清晰和治理保障的不落地,以及域外大国的介入和国际组织发挥的作用有限,共同造成南海海洋治理的困境。2）南海海洋治理以自然海洋与人文海洋的统一为治理客体,以主权国家为最主要的行为主体,需要国家主体间的协同治理。3）从墨家哲学中提取1个核心要点、3个指导要义和4个关键要素,应用于南海海洋治理。在战略功能上以“兼爱非攻”和“义利一体”为价值取向,打破现实主义国际关系局限,以“功利主义”和“志功合一”为行为标准,促进新型国际关系合作;在实操路径上,要嵌入墨家哲学的“法”要素,以规范和标准为牵引,并嵌入墨家哲学的“求”“节”“巧”要素,以科技创新为驱动。  相似文献   

On the contribution of Rossby waves driven by surface buoyancy fluxes to low-frequency North Atlantic steric sea surface height variations          下载免费PDF全文

Peter Kowalski 《大气和海洋科学快报》2022,15(3):100153

Previous studies have shown that wind-forced baroclinic Rossby waves can capture a large portion of low-frequency steric sea surface height (SSH) variations in the North Atlantic. In this paper, the classical wind-driven Rossby wave model derived in a 1.5-layer ocean is extended to include surface buoyancy forcing, and the new model is then used to assess the contribution from buoyancy-forced Rossby waves to low-frequency North Atlantic steric SSH variations. Buoyancy forcing is determined from surface heating as freshwater fluxes are negligible. It is found that buoyancy-forced Rossby waves are important in only a few regions belonging to the subtropical-to-midlatitude and eastern subpolar North Atlantic. In these regions, the new Rossby wave model accounts for 25%–70% of low-frequency steric SSH variations. Furthermore, as part of the analysis it is also shown that a simple static model driven by local surface heat fluxes captures 60%–75% of low-frequency steric SSH variations in the Labrador Sea, which is a region where Rossby waves are found to have no influence on the steric SSH.  相似文献   

气候变化与海洋生态系统：影响、适应和脆弱性——IPCC AR6 WGⅡ报告之解读          下载免费PDF全文

谭红建  蔡榕硕  杜建国  胡文佳 《大气科学学报》2022,45(4):489-501

IPCC第六次评估报告(AR6)第二工作组报告第三章开展了气候变化对海洋的影响和风险,以及生态系统及其服务功能、脆弱性和适应评估。AR6明确指出,人为气候变化已经并将继续显著地改变全球和区域海洋的气候影响驱动因子,包括海温升高、海平面上升、海洋酸化和缺氧,以及营养盐浓度变化等海洋物理和化学因子。例如,20世纪80年代以来全球海洋热浪发生的频率已增加了1倍,到21世纪末期可能增加4～8倍。气候影响驱动因子的变化已经对海洋和海岸带生态系统造成了广泛而深远的影响:1)海洋变暖使得海洋物种自1950年代以来以(59.2±15.5) km/(10 a)的速率向极地方向迁移,导致热带海域生物量减少,中纬度海区热带化,极地和亚极地海区浮游植物生长期提前;2)频繁发生的海洋热浪事件已经接近甚至超过了某些海洋生物的耐受极限或其气候临界点,如暖水珊瑚的大规模白化、死亡,海草和大型海藻的大面积消失;3)海洋变暖、缺氧和酸化使得河口区生物群落结构改变,赤潮等有害藻华事件频发,近海和大洋浮游植物生物量和初级生产力下降;4)海平面上升导致海岸带红树林、盐沼和海草床等生态系统的退化;5)未来全球海洋生态系统面临的风险将不断加剧,尤其是在热带和北冰洋海区。其中,当全球升温1.5℃时(最快到21世纪40年代,SSP5-8.5情景),暖水珊瑚礁预计将减少70％～90％;当升温2℃时,几乎所有的(>99％)暖水珊瑚礁将会消失。目前人类社会采取的一些措施(如建立海洋保护区和红树林生态修复)已越来越不能应对日益增长的气候风险,迫切需要发展变革性的行动措施,推动海洋生态系统恢复力的发展,并需尽快采取强有力的减排措施以减缓全球变暖的影响。  相似文献   

On the determination of the absolute velocity of steady flows of a baroclinic fluid with applications to ocean currents     

《Dynamics of Atmospheres and Oceans》2021

The problem of determining the absolute velocity of marine currents, including its barotropic component, is revisited. A generalization of the classical Needler’s formula is discussed for a Boussinesq fluid and it is shown that the steady flow solution can be deduced from a variational principle that uses the constants of motion existing in the problem. A simple model of a steady flow is considered when the Bernoulli function consists of two terms. The first term is proportional to the square of Ertel’s potential vorticity and the second term is a quadratic function of the fluid buoyancy. This model is applied to mimic the circulation in the western Mediterranean Sea near the African coast. Alternatively, “potential temperature – salinity” coordinates are applied to construct the stream-tubes and infer the steady flow velocity in the simplest case of the Bernoulli function being proportional to the product of the above two variables.  相似文献   

ENSO-7赤道西太平洋异常纬向风所驱动的热带太平洋次表层海温距平的循环   总被引：13，自引：0，他引：13  

李崇银  穆明权 《地球科学进展》2002,17(5):631-638

近几年的一系列分析研究表明，ENSO与异常东亚冬季风之间有相互影响，持续的强（弱）东亚冬季风通过引起赤道西太平洋地区的西（东）风异常对El Niño/La Niña的发生起着重要作用；赤道太平洋次表层海温异常（SOTA）的年际变化（循环）与ENSO发生有密切关系；ENSO的真正源在西太平洋暖池，暖池正（负）SOTA沿赤道温跃层东传到东太平洋，便导致El Niño/La Niña的爆发；在暖池正（负）SOTA沿赤道东传的同时，有负（正）SOTA沿10°N和10°S纬度带向西传播，从而构成SOTA的循环；热带太平洋SOTA循环的驱动者是赤道西太平洋的异常纬向风。进而可以认为：ENSO实质上是主要由异常东亚季风引起的赤道西太平洋异常纬向风所驱动的热带太平洋次表层海温距平的年际循环。  相似文献   

A climate-informed,ecosystem approach to fisheries management     

《Marine Policy》2015

This paper outlines the benefits of using the framework for an ecosystem approach to fisheries management (EAFM) for dealing with the inevitable yet unclear impacts of climate change and ocean acidification on coastal fisheries. With a focus on the Asia-Pacific region, it summarizes the projected biological and socio-economic effects of increased emissions of carbon dioxide (CO₂) for coastal fisheries and illustrates how all the important dimensions of climate change and ocean acidification can be integrated into the steps involved in the EAFM planning process. The activities required to harness the full potential of an EAFM as an adaptation to climate change and ocean acidification are also described, including: provision of the necessary expertise to inform all stakeholders about the risks to fish habitats, fish stocks and catches due to climate change; promotion of trans-disciplinary collaboration; facilitating the participation of all key stakeholders; monitoring the wider fisheries system for climate impacts; and enhancing resources and capacity to implement an EAFM. By channeling some of the resources available to the Asia-Pacific region to adapt to climate change into an EAFM, developing countries will not only build resilience to the ecological and fisheries effects of climate change, they will also help address the habitat degradation and overfishing presently reducing the productivity of coastal fisheries.  相似文献   

一种新的地理本体构建方法分析     

王海涛  刘海砚  尉伯虎  王小军 《测绘科学》2013,38(3)

对于地理本体的研究是在考虑地理信息自身特殊性的基础上,把本体在信息科学中的含义移植到地理信息科学中,实现对空间信息语义的丰富。目前没有一个标准的地理本体构造方法。本文针对当前地理本体构建方法的不足,提出了一种新的地理本体构建方法。该方法强调需求分析的重要性,采用螺旋式上升的构建过程,构建了海运领域地理本体,实现了海运地理信息的语义共享。  相似文献   

Improvement of theories and methods in geodetic joint inversion     

Xu Caijun 《地球空间信息科学学报》2013,16(1):12-18

This paper first establishes the prior globe dynamical model by geophysics, which is a solid earth elastic deformation model. Then, the parameters of the globe dynamic model can be obtained by inverting the geodetic data. The inverse method can be used in seismology and geology, and to make earth-quake prediction.  相似文献   

Quasigeostrophic planetary waves in a two-layer ocean with one-dimensional periodic bottom topography     

Atsushi Kubokawa 《地球物理与天体物理流体动力学》2013,107(2):119-137

Although the study of topographic effects on the Rossby waves in a stratified ocean has a long history, the wave property over a periodic bottom topography whose lateral scale is comparable to the wavelength is still not clear. The present paper treats this problem in a two-layer ocean with one-dimensional periodic bottom topography by a simple numerical method, in which no restriction on the wavelength and/or the horizontal scale of the topography is required. The dispersion diagram is obtained for a wavenumber range of [?π/L _b , π/L _b ], where L _b is the periodic length of the topography. When the topographic?β?is not negligible compared to the planetary β, the Rossby wave solutions around the wavenumbers which satisfy the resonant condition among the waves and topography disappear and separate into an infinite number of discrete modes. For convenience, each mode is numbered in order of frequency. As topographic height is increased, the high frequency barotropic Rossby wave (mode 1) becomes a topographic mode which can exist even on the f plane, and the highfrequency baroclinic mode (mode 2) becomes a surface intensified mode. Behaviors of low frequency modes are somewhat complicated. When the topographic amplitude is small, the low frequency baroclinic modes tend to be bottom trapped and the low frequency barotropic modes tend to be surface intensified. As topographic amplitude further increases, the relation between the mode number and vertical structure changes. This change can be attributed to the increase of the frequency of the topographic mode with the topographic amplitude.  相似文献