Catalogue Search | MBRL
Search Results Heading
Explore the vast range of titles available.
MBRLSearchResults
-
DisciplineDiscipline
-
Is Peer ReviewedIs Peer Reviewed
-
Series TitleSeries Title
-
Reading LevelReading Level
-
YearFrom:-To:
-
More FiltersMore FiltersContent TypeItem TypeIs Full-Text AvailableSubjectPublisherSourceDonorLanguagePlace of PublicationContributorsLocation
Done
Filters
Reset
8,474
result(s) for
"Maritime boundaries."
Sort by:
The South China Sea disputes : past, present, and future
\"This study provides political and economic analyses of current controversies in the South China Sea. It examines enduring territorial disputes, competing maritime claims, and the historical roots of regional mistrust. It also analyzes how such antagonisms affect the regional security structure and offers solutions to resolve the conflicts\"-- Provided by publisher.
The Channel : England, France and the Construction of a Maritime Border in the Eighteenth Century
\"Rather than a natural frontier between natural enemies, this book approaches the English Channel as a shared space, which mediated the multiple relations between France and England in the long eighteenth century, in both a metaphorical and a material sense. Instead of arguing that Britain's insularity kept it spatially and intellectually segregated from the Continent, Renaud Morieux focuses on the Channel as a zone of contact. The 'narrow sea' was a shifting frontier between states and a space of exchange between populations. This richly textured history shows how the maritime border was imagined by cartographers and legal theorists, delimited by state administrators and transgressed by migrants. It approaches French and English fishermen, smugglers and merchants as transnational actors, whose everyday practices were entangled. The variation of scales of analysis enriches theoretical and empirical understandings of Anglo-French relations, and reassesses the question of Britain's deep historical connections with Europe\"-- Provided by publisher.
The South China Sea disputes
2016,2018
The South China Sea has long been regarded as one of the most complex and challenging ocean-related maritime disputes in East Asia.Recently it has become the locus of disputes that have the potential of escalating into serious international conflicts.
China's troubled waters : maritime disputes in theoretical perspective
\"How are China's ongoing sovereignty disputes in the East and South China Seas likely to evolve? Are relations across the Taiwan Strait poised to enter a new period of relaxation or tension? How are economic interdependence, domestic public opinion, and the deterrence role played by the US likely to affect China's relations with its counterparts in these disputes? Although territorial disputes have been the leading cause for interstate wars in the past, China has settled most of its land borders with its neighbours. Its maritime boundaries, however, have remained contentious. This book examines China's conduct in these maritime disputes in order to analyse Beijing's foreign policy intentions in general. Rather than studying Chinese motives in isolation, Steve Chan uses recent theoretical and empirical insights from international relations research to analyse China's management of its maritime disputes\"-- Provided by publisher.
Much Ado about Something: The Tiran and Sanafir Islands in International, Regional and Domestic Politics (1841–2023)
2025
The Tiran and Sanafir are two small arid and uninhabited islands at the mouth of the Gulf of 'Aqaba, close to the Egyptian and Saudi shores. Their importance derives from their strategic location at the entrance to the Gulf of Aqaba and the maritime route to Jordan's port Aqaba and Israel's port Eilat. Since the 19th century, they have played an important role in international, regional and domestic politics, with the involvement of numerous actors: the Ottoman Empire, Britain, Italy, the United States, the kingdom of Hijaz, Egypt, Saudi Arabia, Jordan, Israel and the United Nations. The aim of this article is to explore the micro-history of the Tiran and Sanafir islands, as well as the Tiran Straits, as a center of power politics. It would show that what started as an international dispute between Britain and the Ottoman Empire, turned into a regional conflict within the Arab-Israeli conflict, and finally ended as a heated issue in Egyptian domestic politics, affecting also Egyptian-Saudi relations. In 2023, with the return of the islands to their original owner—Saudi Arabia—a two centuries long conflict came to an end.
Journal Article
The South China Sea : a crucible of regional cooperation or conflict-making sovereignty claims?
\"As a primary trade route for more than half of the world's shipping, the location of potentially huge oil and gas reserves, and the main source of protein in maritime South- East Asia, the South China Sea is a governing determinant of security, prosperity and development in East Asia and the wider Indo-Pacific region. The disputes in the South China Sea have long been seen as a source of tension and instability in the region. Although peace has been maintained until now, the South China Sea is the epicentre of changes in the international balance of power which have the potential to trigger military conflict. The South China Sea sovereignty disputes are among the most complicated in the world and engage claims from Brunei, China, Malaysia, Philippines, Taiwan, and Vietnam. Given the complex convergence of national interests in the region, the prospect of settling the decades-old disputes completely is very slim\"-- Provided by publisher.
Review of Wind–Wave Coupling Models for Large-Eddy Simulation of the Marine Atmospheric Boundary Layer
by
Draxl, Caroline
,
Lee, Joseph C. Y.
,
Sprague, Michael A.
in
Air-sea interaction
,
Atmospheric boundary layer
,
Atmospheric models
2021
We present a review of existing wind–wave coupling models and parameterizations used for large-eddy simulation of the marine atmospheric boundary layer. The models are classified into two main categories: (i) the wave-phase-averaged, sea surface–roughness models and (ii) the wave-phase-resolved models. Both categories are discussed from their implementation, validity, and computational efficiency viewpoints, with emphasis given on their applicability in offshore wind energy problems. In addition to the various models discussed, a review of laboratory-scale and field-measurement databases is presented thereafter. The majority of the presented data have been gathered over many decades of studying air–sea interaction phenomena, with the most recent ones compiled to reflect an offshore wind energy perspective. Both provide valuable data for model validation. We also discuss the modeling knowledge gaps and computational challenges ahead.
Journal Article
Marine Boundary Layers above Heterogeneous SST: Across-Front Winds
by
Weil, Jeffrey C.
,
Sullivan, Peter P.
,
McWilliams, James C.
in
Advection
,
Atmospheric boundary layer
,
Blowing time
2020
Turbulent flow in a weakly convective marine atmospheric boundary layer (MABL) driven by geostrophic winds U g = 10 m s −1 and heterogeneous sea surface temperature (SST) is examined using fine-mesh large-eddy simulation (LES). The imposed SST heterogeneity is a single-sided warm or cold front with temperature jumps Δ θ = (2, −1.5) K varying over a horizontal distance between [0.1, −6] km characteristic of an upper-ocean mesoscale or submesoscale regime. A Fourier-fringe technique is implemented in the LES to overcome the assumptions of horizontally homogeneous periodic flow. Grid meshes of 2.2 × 10 9 points with fine-resolution (horizontal, vertical) spacing ( δx = δy , δz ) = (4.4, 2) m are used. Geostrophic winds blowing across SST isotherms generate secondary circulations that vary with the sign of the front. Warm fronts feature overshoots in the temperature field, nonlinear temperature and momentum fluxes, a local maximum in the vertical velocity variance, and an extended spatial evolution of the boundary layer with increasing distance from the SST front. Cold fronts collapse the incoming turbulence but leave behind residual motions above the boundary layer. In the case of a warm front, the internal boundary layer grows with downstream distance conveying the surface changes aloft and downwind. SST fronts modify entrainment fluxes and generate persistent horizontal advection at large distances from the front.
Journal Article