Relevant bibliographies by topics / Maritime continent

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Maritime continent'

Author: Grafiati
Published: 4 June 2021
Last updated: 2 February 2022

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Journal articles on the topic "Maritime continent"

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Tabrani, Primadi. "INFO INFO YANG MENDEBARKAN: Punden Berundak, Toba Purba, Banjir Besar, Wawasan Nusantara, Gunung Padang." Jurnal Budaya Nusantara 1, no. 2 (2014): 102–20. http://dx.doi.org/10.36456/b.nusantara.vol1.no2.a410.

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This article is not yet a real research; it is more as a deep reflection. But those deep reflections are worth to be researched thoroughly by experts from many fields of study integratingly. Thinking of people in land-continent with many countries as Europe is different then thinking of people in one country as Indonesia, a maritime-continent. In land-continents thinking, sea is to separte, in maritime-continent Indonesia with its islands, sea is to unite, wawasan Nusantara as old as prehistory. Each countryin a land-continent are eager to differentiate and defend to other countries by ethnic, language, religion, ideology, while in Indonsia as a maritime-continent, we is one country, several parts are slightly different but we are “one”: “Bhinneka Tunggal Ika”. In land-continent countries, a city with walls fortification, a country with great walls fortification are usual. While it is not so in Maritime-continent Indonesia, as is Trowulan the capital of the great empire Majapahit. Our school books says that the population of Indonesia comes from Asia, 5000 BC and 2000BC, while it is known that the migration of homosapiens has reach West Nusantara about 60 – 80.000 BC, and experienced the ancient Toba Mountain great explosion and the three great floods.The west theory said that Indonesia is a country between two continents and two aceans, where culture, etnic, nation, religion, etc, criss cross ofer it. So Indonesia ’has nothing’. No local genius. Nusantara people cruises the Pacific and Indian ocean before Christ, the Atlantic in the first century. What about ”Atlantis” and ”Eden in the East” situated in Sundaland, that alter the world culture, history & development? Has all this a connection with the mistery of Gunung Padang? Keywords: Land-continent thinking, Maritime-continent thinking, Wawasan Nusantara, BhinnekaTunggal Ika, Gunung Padang.
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Lee, Shao-Yi, and John L. McBride. "The progression of the boreal winter monsoon through the western Maritime Continent as differentiated by ENSO phase." Advances in Geosciences 42 (August 24, 2016): 51–60. http://dx.doi.org/10.5194/adgeo-42-51-2016.

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Abstract. The impact of global ENSO on the regional monsoon onset over the Maritime Continent is examined, using satellite-derived scatterometer surface winds over the sea channel from the South China Sea, through the Karimata Strait into the Java Sea. An index of monsoon onset, fracsign, is defined based on a positive dot-product between the monthly wind at each gridpoint and the "basis-wind" or climatological wind at the peak of the relevant monsoon season.Rather than being delayed throughout the Maritime Continent during El Niño years, the monsoon is seen to arrive faster at and remain longer over the western Maritime Continent, and therefore delayed for the eastern Maritime Continent. The wind-based diagnostic can be further decomposed into two components that reflect the monsoon wind strength and the location of the wind convergence zone, respectively. During El Niño years, the monsoon strength post-onset is weaker than normal over the eastern maritime continent. However, there is no ENSO-related differentiation in monsoon strength post-onset over the western Maritime Continent.
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Kucienska, B., G. B. Raga, and R. Romero-Centeno. "High lightning activity in maritime clouds near Mexico." Atmospheric Chemistry and Physics 12, no. 17 (2012): 8055–72. http://dx.doi.org/10.5194/acp-12-8055-2012.

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Abstract. Lightning activity detected by the World Wide Lightning Location Network (WWLLN) over oceanic regions adjacent to Mexico is often as high as that observed over the continent. In order to explore the possible causes of the observed high flash density over those regions, the relationships between lightning, rainfall, vertical hydrometeor profiles, latent heating, wind variability and aerosol optical depth are analyzed. The characteristics of lightning and precipitation over four oceanic zones adjacent to Mexican coastlines are contrasted against those over the continent. The number of flashes per rainfall over some coastal maritime regions is found to be higher than over the continent. The largest number of flashes per rainfall is observed during the biomass burning season. In addition, we compare two smaller areas of the Tropical Pacific Ocean: one located within the Inter-Tropical Convergence Zone and characterized by high rainfall and weak lightning activity and the other one influenced by a continental wind jet and characterized by high rainfall and strong lightning activity. During the rainy season, the monthly distribution of lightning within the region influenced by the continental wind jet is contrary to that of rainfall. Moreover, the monthly variability of lightning is very similar to the variability of the meridional wind component and it is also related to the variability of aerosol optical depth. The analysis suggests that the high lightning activity observed over coastal Pacific region is linked to the continental cloud condensation nuclei advected over the ocean. Analysis of daily observations indicates that the greatest lightning density is observed for moderate values of the aerosol optical depth, between 0.2 and 0.35.
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Wu, Cheng-Han, and Huang-Hsiung Hsu. "Topographic Influence on the MJO in the Maritime Continent." Journal of Climate 22, no. 20 (2009): 5433–48. http://dx.doi.org/10.1175/2009jcli2825.1.

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Abstract This study demonstrates that during the passage of the MJO through the Maritime Continent in the boreal winter, the corresponding deep convection and near-surface wind anomalies tend to skirt around mountainous islands. Flow bifurcation around elongated mountainous islands, such as New Guinea, is clearly seen. Topographic blocking generates distinctive vorticity and convergence distributions in this specific domain. Mountain-wave-like structures are also observed throughout the Maritime Continent, with a clear spatial relationship with the high terrains in Sumatra, Sulawesi, and New Guinea. The existence of topography seems to create extra lifting and sinking within the large-scale circulation and thus the convective system exhibits quasi-stationary features near the major topography during the MJO passage through the Maritime Continent. It is suggested that resolving the detailed topographic effects may play a key role in simulating realistic characteristics of the MJO in the Maritime Continent.
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Kucienska, B., G. B. Raga, and R. Romero-Centeno. "High lightning activity in maritime clouds near Mexico." Atmospheric Chemistry and Physics Discussions 12, no. 1 (2012): 2817–52. http://dx.doi.org/10.5194/acpd-12-2817-2012.

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Abstract. Lightning activity detected by the World Wide Lightning Location Network (WWLLN) over oceanic regions adjacent to Mexico is often as high as that observed over the continent. In order to explore the possible cause of the observed high flash density over those regions, the relationships between lightning, rainfall, vertical hydrometeor profiles, latent heating, wind variability and aerosol optical thickness are analyzed. The characteristics of lightning and precipitation over four oceanic zones adjacent to Mexican coastlines are contrasted against those over the continent. In addition, we compare two smaller regions over the Tropical Pacific Ocean: one located within the Inter-Tropical Converge Zone and characterized by high rainfall and weak lightning activity and the other influenced by a continental jet and presenting high rainfall and strong lightning activity over the Gulf of Tehuantepec. Maritime precipitating clouds that develop within the region influenced by offshore winds exhibit similar properties to continental clouds: large content of precipitation ice and an increased height range of coexistence of precipitation ice and cloud water. During the rainy season, monthly distribution of lightning within the region influenced by the continental jet is contrary to that of rainfall. Moreover, the monthly variability of lightning is very similar to the variability of the meridional wind component and it is also related to the variability of aerosol optical depth. The analysis strongly suggests that the high lightning activity observed over the Gulf of Tehuantepec is caused by continental cloud condensation nuclei advected over the ocean.
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Sherwood, Steven C. "A stratospheric “drain” over the maritime continent." Geophysical Research Letters 27, no. 5 (2000): 677–80. http://dx.doi.org/10.1029/1999gl010868.

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Simpson, J., Th D. Keenan, B. Ferrier, R. H. Simpson, and G. J. Holland. "Cumulus mergers in the maritime continent region." Meteorology and Atmospheric Physics 51, no. 1-2 (1993): 73–99. http://dx.doi.org/10.1007/bf01080881.

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Qian, Jian-Hua. "Why Precipitation Is Mostly Concentrated over Islands in the Maritime Continent." Journal of the Atmospheric Sciences 65, no. 4 (2008): 1428–41. http://dx.doi.org/10.1175/2007jas2422.1.

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Abstract High-resolution observations and regional climate model simulations reveal that precipitation over the Maritime Continent is mostly concentrated over islands. Analysis of the diurnal cycles of precipitation and winds indicates that this is predominantly caused by sea-breeze convergence over islands, reinforced by mountain–valley winds and further amplified by the cumulus merger processes. Comparison of a regional climate model control simulation to a flat-island run and an all-ocean run demonstrates that the underrepresentation of islands and terrain in the Maritime Continent weakens the atmospheric disturbance associated with the diurnal cycle, and hence underestimates precipitation. The implication of these regional modeling results is that systematic errors in coarse-resolution global circulation models probably result from insufficient representation of land–sea breezes associated with the complex topography in the Maritime Continent. It is found that precipitation in the Maritime Continent, simulated by a global model, is indeed smaller than observed. The simulated upper-atmospheric velocity potential, which represents large-scale tropospheric heating, was substantially displaced eastward compared to observations. Possible approaches toward solving this problem are suggested.
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Hu, Chundi, Tao Lian, Ho-Nam Cheung, et al. "Mixed diversity of shifting IOD and El Niño dominates the location of Maritime Continent autumn drought." National Science Review 7, no. 7 (2020): 1150–53. http://dx.doi.org/10.1093/nsr/nwaa020.

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Summary The Maritime Continent is a huge heat source region over the Indo-Pacific warm pool and it plays a key role in global weather/climate variations. The locations of Maritime Continent autumn droughts, linked to frequent rampant forest wildfires, are closely related to the mixed diversity of El Niño and Indian Ocean Dipole events.
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Tenório, Ricardo Sarmento, Marcia Cristina da Silva Moraes, and Henri Sauvageot. "Raindrop Size Distribution and Radar Parameters in Coastal Tropical Rain Systems of Northeastern Brazil." Journal of Applied Meteorology and Climatology 51, no. 11 (2012): 1960–70. http://dx.doi.org/10.1175/jamc-d-11-0121.1.

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AbstractA dataset on raindrop size distribution (DSD) gathered in a coastal site of the Alagoas state in northeastern Brazil is used to analyze some differences between continental and maritime rainfall parameters. The dataset is divided into two subsets. One is composed of rainfall systems coming from the continent and moving eastward (i.e., offshore), representing the continental subset. The other is composed of rainfall systems that developed over the sea and are moving westward (i.e., inshore), representing the maritime subset. The mean conditional rain rate (i.e., for rain rate R > 0) is found to be higher for maritime (4.6 mm h−1) than for continental (3.2 mm h−1) conditions. The coefficient of variation of the conditional rain rate is lower for the maritime (1.75) than for the continental (2.25) subset. The continental and maritime DSDs display significant differences. For drop diameter D smaller than about 2 mm, the number of drops is higher for maritime rain than for continental rain. This reverses for D > 2 mm, in such a way that radar reflectivity factor Z for the maritime case is lower than for the continental case at the same rain rate. These results show that, to estimate precipitation by radar in the coastal area of northeastern Brazil, coefficients of the Z–R relation need to be adapted to the direction of motion of the rain-bearing system, inshore or offshore.
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Dissertations / Theses on the topic "Maritime continent"

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Strachan, Jane. "Understanding and modelling the climate of the Maritime Continent." Thesis, University of Reading, 2007. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.494989.

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The Maritime Continent has been identified as a region of major climatic importance on both local and global scales. It is essential that the region is sufficiently represented in GCMs in order to correctly reproduce observed regional climatology and ultimately global circulation. However, the region represents a major modelling challenge. Systematic underestimation of precipitation over the Maritime Continent region is experienced in many atmosphere-only general circulation models (AGCMs), including the Hadley Centre Global Atmospheric Model (HadGAMl). The discrepancy in rainfall leads to errors not only in the Maritime Continent region, but to systematic errors elsewhere, both in the tropics and extra-tropics.
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Hamada, Junichi. "A Climatological Study on Rainfall Variations over the Indonesian Maritime Continent." 京都大学 (Kyoto University), 2003. http://hdl.handle.net/2433/149072.

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Ashfold, Matthew James. "Short-lived halocarbons in the atmosphere of the maritime continent : sources and transport." Thesis, University of Cambridge, 2013. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.607852.

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Gianotti, Rebecca L. (Rebecca Louise). "Convective cloud and rainfall processes over the Maritime Continent : simulation and analysis of the diurnal cycle." Thesis, Massachusetts Institute of Technology, 2012. http://hdl.handle.net/1721.1/79488.

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Thesis (Ph. D. in the Field of Hydrology)--Massachusetts Institute of Technology, Dept. of Civil and Environmental Engineering, February 2013.<br>"February 2013." Cataloged from PDF version of thesis.<br>Includes bibliographical references (p. 290-307).<br>The Maritime Continent experiences strong moist convection, which produces significant rainfall and drives large fluxes of heat and moisture to the upper troposphere. Despite the importance of these processes to global circulations, current predictions of climate change over this region are still highly uncertain, largely due to inadequate representation of the diurnally-varying processes related to convection. In this work, a coupled numerical model of the land-atmosphere system (RegCM3-IBIS) is used to investigate how more physically-realistic representations of these processes can be incorporated into large-scale climate models. In particular, this work improves simulations of convective-radiative feedbacks and the role of cumulus clouds in mediating the diurnal cycle of rainfall. Three key contributions are made to the development of RegCM3-IBIS. Two pieces of work relate directly to the formation and dissipation of convective clouds: a new representation of convective cloud cover, and a new parameterization of convective rainfall production. These formulations only contain parameters that can be directly quantified from observational data, are independent of model user choices such as domain size or resolution, and explicitly account for subgrid variability in cloud water content and nonlinearities in rainfall production. The third key piece of work introduces a new method for representation of cloud formation within the boundary layer. A comprehensive evaluation of the improved model was undertaken using a range of satellite-derived and ground-based datasets, including a new dataset from Singapore's Changi airport that documents diurnal variation of the local boundary layer height. The performance of RegCM3-IBIS with the new formulations is greatly improved across all evaluation metrics, including cloud cover, cloud liquid water, radiative fluxes and rainfall, indicating consistent improvement in physical realism throughout the simulation. This work demonstrates that: (1) moist convection strongly influences the near surface environment by mediating the incoming solar radiation and net radiation at the surface; (2) dissipation of convective cloud via rainfall plays an equally important role in the convective-radiative feedback as the formation of that cloud; and (3) over parts of the Maritime Continent, rainfall is a product of diurnally-varying convective processes that operate at small spatial scales, on the order of 1 km.<br>by Rebecca L. Gianotti.<br>Ph.D.in the Field of Hydrology
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Kuznetsova, Daria. "Modélisation de l'oscillation Madden-Julian lors de son passage sur l'océan Indien et le continent maritime." Thesis, Toulouse 3, 2018. http://www.theses.fr/2018TOU30220/document.

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L'oscillation de Madden-Julian (MJO) est la composante dominante de la variabilité intrasaisonnière dans l'atmosphère tropicale, se propageant vers l'est dans la bande équatoriale. Elle se compose d'un centre convectif (phase active) accompagné de la convergence des anomalies du vent zonal de bas niveau et de la divergence de niveau supérieur, et de zones de convection faible (phases supprimées). Trois périodes de l'activité MJO sur l'océan Indien et le continent maritime ont été choisies : 6-14 avril 2009, 23-30 novembre 2011 et 9-28 février 2013. Les simulations avec et sans paramétrisation de la convection ont été réalisées pour un grand domaine avec le modèle atmosphérique Méso-NH. Il a été obtenu que les simulations avec convection paramétrée n'étaient pas capables de reproduire un signal MJO. Pour 2009 et 2011, lorsque le couplage entre la convection et la circulation de grande échelle était fort, les simulations avec convection explicite ont montré une propagation visible de la MJO, ce qui n'a pas été le cas pour 2013. Pour 2011, les processus contribuant à la suppression de la convection ont été étudiés avec une analyse isentropique pour séparer les masses d'air ascendantes ayant une température potentielle équivalente élevée des masses d'air subsidentes ayant une température potentielle équivalente faible. Trois circulations de grande échelle ont été trouvées : une circulation troposphérique, une circulation de percées nuageuses dans la couche de tropopause tropicale, et une circulation de masses d'air à faible température potentielle équivalente dans la basse troposphère. Cette dernière correspond aux intrusions d'air sec de grande échelle des zones subtropicales dans la bande équatoriale, trouvées principalement pendant la phase supprimée de la MJO sur l'océan Indien<br>The Madden-Julian Oscillation (MJO) is the dominant component of the intraseasonal variability in the tropical atmosphere, propagating eastward in the equatorial band. It consists of a convective center (active phase) accompanied by the low-level zonal wind anomaly convergence and the upper-level zonal wind anomaly divergence, and zones of weak convection (suppressed phases). Three time periods of the MJO activity over the Indian Ocean and the Maritime Continent were chosen: 6-14 April 2009, 23-30 November 2011, and 9-28 February 2013. The simulations with and without convective parameterizations were performed for a large domain with the atmospheric model Méso-NH. It was obtained that the simulations with parameterized convection were not able to reproduce an MJO signal. For 2009 and 2011 when the coupling between convection and large-scale circulation was strong, the convection-permitting simulations showed a visible MJO propagation, which was not the case for 2013. For the 2011 episode, the processes contributing to the suppression of the convection were studied using an isentropic analysis to separate the ascending air masses with high equivalent potential temperature from the subsiding air masses with low equivalent potential temperature. Three large-scale circulations were found: a tropospheric circulation, an overshoot circulation within the tropical tropopause layer, and a circulation of air masses with low equivalent potential temperature in the lower troposphere. The latter corresponds to the large-scale dry air intrusions from the subtropical zones into the equatorial band, mostly found during the suppressed MJO phase over the Indian Ocean
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Peatman, Simon. "The Madden-Julian Oscillation and the diurnal cycle over the Maritime Continent : scale interactions and modelling." Thesis, University of East Anglia, 2014. https://ueaeprints.uea.ac.uk/48786/.

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The Maritime Continent archipelago, situated on the equator at 95-165E, has the strongest land-based precipitation on Earth. The latent heat release associated with the rainfall affects the atmospheric circulation throughout the tropics and into the extra-tropics. The greatest source of variability in precipitation is the diurnal cycle. The archipelago is within the convective region of the Madden-Julian Oscillation (MJO), which provides the greatest variability on intra-seasonal time scales: large-scale (∼10^7 km^2) active and suppressed convective envelopes propagate slowly (∼5 m s^-1) eastwards between the Indian and Pacific Oceans. High-resolution satellite data show that a strong diurnal cycle is triggered to the east of the advancing MJO envelope, leading the active MJO by one-eighth of an MJO cycle (∼6 days). Where the diurnal cycle is strong its modulation accounts for 81% of the variability in MJO precipitation. Over land this determines the structure of the diagnosed MJO. This is consistent with the equatorial wave dynamics in existing theories of MJO propagation. The MJO also affects the speed of gravity waves propagating offshore from the Maritime Continent islands. This is largely consistent with changes in static stability during the MJO cycle. The MJO and its interaction with the diurnal cycle are investigated in HiGEM, a high-resolution coupled model. Unlike many models, HiGEM represents the MJO well with eastward-propagating variability on intra-seasonal time scales at the correct zonal wavenumber, although the inter-tropical convergence zone's precipitation peaks strongly at the wrong time, interrupting the MJO's spatial structure. However, the modelled diurnal cycle is too weak and its phase is too early over land. The modulation of the diurnal amplitude by the MJO is also too weak and accounts for only 51% of the variability in MJO precipitation. Implications for forecasting and possible causes of the model errors are discussed, and further modelling studies are proposed.
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Kwiatkowski, Cornelia Regula Verfasser], Mahyar [Akademischer Betreuer] [Mohtadi, Dierk [Gutachter] Hebbeln, and Heiko [Gutachter] Pälike. "Mid- to late Holocene climate variability of the Maritime Continent / Cornelia Regula Kwiatkowski ; Gutachter: Dierk Hebbeln, Heiko Pälike ; Betreuer: Mahyar Mohtadi." Bremen : Staats- und Universitätsbibliothek Bremen, 2016. http://d-nb.info/1123194750/34.

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Chandrasa, Ganesha Tri. "Evaluation of Regional Climate Model Simulated Rainfall over Indonesia and its Application for Downscaling Future Climate Projections." The Ohio State University, 2018. http://rave.ohiolink.edu/etdc/view?acc_num=osu1523464961178694.

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Heisten, Laurent. "De aequitate in delimitatione maritima : l’équité dans la délimitation maritime : essai sur une théorisation de la jurisprudence internationale en matière de délimitation maritime équitable." Thesis, Paris 10, 2016. http://www.theses.fr/2016PA100196/document.

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Dès le premier arrêt rendu en matière de délimitation du plateau continental et de la zone économique exclusive, la jurisprudence internationale se fonde sur le concept de l’équité en vue de tracer les frontières maritimes. Elle a progressivement développé des règles gouvernant la délimitation maritime équitable et qui peuvent être classées en quatre catégories de normes, qui sont la norme fondamentale requérant la recherche d’un résultat équitable, les principes équitables, les méthodes de délimitation maritime et les circonstances pertinentes qui permettent d’adapter une ligne de délimitation provisoirement arrêtée aux circonstances de l’espèce. Ces règles devraient toutes contribuer à l’obtention d’un résultat équitable.Les règles visées ont peu à peu accédé à la normativité, ce qui permet de distinguer entre quatre degrés de normativité dans l’évolution du droit relatif à la délimitation maritime équitable. Au degré zéro de normativité, le droit était réduit à la norme fondamentale et, par la suite, les principes équitables et les méthodes de délimitation ont accédé à la normativité. Leur normativisation permet de distinguer entre les degrés premier et deuxième de normativité. Le degré supérieur de normativité serait qualifié par la normativité de tous les facteurs de délimitation, y compris les circonstances pertinentes.La détermination de ces règles se fonde sur l’idée d’équité. Comme cette équité est requise par la norme fondamentale, il faut parler d’une équité juridique. Elle est un moyen autonome qui permet de compléter le droit de la délimitation maritime. Avec le développement progressif de ce droit, l’équité juridique (aequitas iuridicia) perd en influence et est remplacée par l’équité qui est une composante des normes (aequitas elementum iuris). Cette dernière dirige l’interprétation des normes de délimitation en vue de parvenir à un résultat équitable. Une pratique jurisprudentielle abondante a contribué à cette évolution qui se caractérise par la mise à l’écart de l’équité juridique<br>Since the first decision related to the delimitation of the continental shelf and the exclusive economic zone, the international jurisprudence is founded on the concept of equity. The international jurisprudence has progressively developed rules governing the equitable maritime delimitation, which can be classified in four categories of norms: the fundamental norm requiring the adoption of an equitable result, equitable principles, delimitation methods and relevant circumstances that contribute to adapt the provisional delimitation line on the concrete circumstances of the case. All those rules should contribute to the adoption of an equitable result.The rules mentioned above acceded progressively on normativity, which permits to distinguish four degrees of normativity in the evolution of the law applicable on equitable maritime delimitation. On degree zero of normativity, law was reduced on the fundamental norm and, thereafter, equitable principles and delimitation acceded on normativity. Their normativisation permits to distinguish between the first and the second degree of normativity. The superior degree of normativity is qualified by the normativity of all delimitation factors, even the relevant circumstances.The determination of these rules is based on the idea of equity. As the fundamental norm requires this equity, it should be called juridical equity. It is an autonomous tool, which completes the law applicable on maritime delimitation. Through the progressive development of the law, juridical equity (aequitas iuridicia) looses its influence and is replaced by equity that is a part of the norms (aequitas elementum iuris). This one guides the interpretation of the delimitation norms in order to obtain an equitable result. An abundant juridical practice has contributed to this evolution characterised by the rejection of juridical equity
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Martins, José Roberto Serra 1965. "Plataforma Continental Juridica = incorporação ao territorio nacional e ao ensino de Geociencias." [s.n.], 2010. http://repositorio.unicamp.br/jspui/handle/REPOSIP/287221.

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Orientador: Celso Dal Re Carneiro<br>Dissertação (mestrado) - Universidade Estadual de Campinas, Instituto de Geociencias<br>Made available in DSpace on 2018-08-15T15:40:36Z (GMT). No. of bitstreams: 1 Martins_JoseRobertoSerra_M.pdf: 2357471 bytes, checksum: 19beeda9b140e61ad2baf860519a183a (MD5) Previous issue date: 2010<br>Resumo: O objetivo da pesquisa é produzir material didático capaz de explicar a idéia de Plataforma Continental Jurídica (PCJ) em manuais escolares e atividades de educação básica. A tarefa exige análise direta (1) dos condicionantes geológicos e geomorfológicos sobre as quais estão definidos os critérios de delimitação da PCJ, e (2) do processo pelo qual um país legitima a incorporação da mesma ao respectivo território. Os documentos reunidos salientam resultados sociais, culturais, econômicos e estratégicos que podem ser obtidos pelo Brasil nesse processo, a depender do acolhimento do pleito por parte da Comissão de Limites da Organização das Nações Unidas (ONU). O texto da Convenção das Nações Unidas sobre Direito do Mar (CNUDM) garante aos Estados costeiros a expansão da Plataforma Continental, além do limite de 200 milhas marítimas - limite externo da Zona Econômica Exclusiva (ZEE). Para tanto, o Estado deve realizar levantamentos da margem continental (leito e subsolo marinhos) que comprovem a continuidade do bloco crustal para além dos limites da ZEE. Após o levantamento (LEPLAC, no Brasil), o país deve pleitear à Comissão de Limites da ONU a expansão de direitos sobre recursos minerais da área. A Dissertação contextualiza o tema, segundo ordenação temporal que vai da evolução geológica à da incorporação jurídica. O enfoque é essencialmente histórico: (1) Uma história de milhões de anos: sintetiza os processos geológicos formadores de nossa margem continental; (2) Uma história de milhares de anos: enfoca a relação da humanidade e do processo civilizatório com o mar; (3) Uma história de dezenas de anos: explica os trâmites legais para definição da Plataforma Continental Jurídica, com base em princípios geológicos, históricos e legais. O pleito brasileiro de 4.452.000 km2 amplia em 52 % a área de 8.514.876,6 km2 de terras emersas que compõem o território nacional. O material didático elaborado e testado propõe atividades capazes de desvendar, em sequência, cada aspecto citado. As metas principais são: (1) convidar o leitor a analisar uma situação-problema segundo ângulos diferentes de visão; (2) demonstrar que o processo civilizatório, decorrente de uma história das mentalidades, é parte fundamental para plena compreensão do interesse legal do Estado e (3) comprovar que esses conhecimentos são absolutamente imprescindíveis para plena formação de um cidadão brasileiro, em sintonia com os dias atuais.<br>Abstract: The objective of this research is to produce educational materials capable of explaining the idea of the Extended Continental Shelf (ECS) in textbooks and activities for basic education. It requires direct analysis of: (1) the geological and geomorphological requirements for such definition, and (2) the process by which a given country is capable to declare its ECS. The collected documents highlight social, cultural, economic and strategic results that Brazil may obtain from this process, depending on the acceptance of a case by the Commission on the Limits of the Continental Shelf (UN-CLCS). The text of the UN Convention on the Law of the Sea (UNCLOS) provides for coastal states to expand the Continental Shelf beyond the 200 nautical miles - the outer limit of the Exclusive Economic Zone (EEZ). To this end, the State should carry out surveys of the continental margin (soil, sediments and bedrock) to prove the continuity of the crustal block beyond the limits of the EEZ. After the survey (LEPLAC in Brazil), the country must plead to the UN-CLCS expansion of rights to mineral resources of the area. The dissertation contextualizes the issue, according to a temporal ordering from the geological evolution towards a legal definition. The approach is essentially historical: (1) A history of millions of years: summarizes the forming geological processes of the Brazilian continental margin, (2) A history of thousands of years: focuses on the relationship of humanity and the civilizatory process with the sea, (3) A history of decades: it explains the legal procedures for setting the Extended Continental Shelf, based on geological, historical and legal principles. The Brazilian application of 4,452,000 km2 expands 52% the area of 8,514,876.6 km2 of dry land that compose the country. The developed and tested teaching materials have proposed activities capable of revealing, in sequence, each one of these aspects. The main goals are: (1) to invite the reader to examine a concrete problem under different angles of vision, (2) to show that, due to a history of mentalities, the civilizatory process is key to a complete understanding of the legal interests of a State and (3) to demonstrate that this knowledge is indispensable to educate Brazilian citizens.<br>Mestrado<br>Mestre em Ensino e Historia de Ciencias da Terra
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Books on the topic "Maritime continent"

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Féraud, Pierre-François. Histoire des liaisons maritimes entre le continent et l'île de Groix: Chronique maritime. Atelier Alpha Bleue, 1995.

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Wain, Alan. Air parcel transport over the maritime continent as determined from trajectory climatologies, 1994-1999. School of Geography and Environmental Science, Monash University, 2002.

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Parliament, Great Britain. A bill to repeal an act of the ninth year of His Late Majesty, for regulating the carriage of passengers in merchant vessels from the United Kingdom to the British possessions on the continent and islands of North America, and to make further provision for regulating the same. s.n., 2000.

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Parliament, Great Britain. A bill (as amended on re-commitment) to repeal an act of the ninth year of His Late Majesty, for regulating the carriage of passengers in merchant vessels from the United Kingdom to the British possessions on the continent and islands of North America, and to make further provision for regulating the same. s.n., 2000.

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Maritime strategy and continental wars. F. Cass, 1998.

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Kaye, Stuart. Australia's maritime boundaries. 2nd ed. Centre for Maritime Policy, University of Wollongong, 2001.

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Kaye, Stuart B. Australia's maritime boundaries. Centre for Maritime Policy, University of Wollongong, 1995.

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Relevant circumstances and maritime delimitation. Clarendon Press, 1989.

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Kolb, Robert. Case law on equitable maritime delimitation: Digest and commentaries = Jurisprudence sur les délimitations maritimes selon l'équité : répertoire et commentaries. Kluwer Academic Publishers, 2003.

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Kamga, Maurice K. Délimitation maritime sur la côte atlantique africaine. Bruylant ; Éd. de l'Université de Bruxelles, 2005.

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Book chapters on the topic "Maritime continent"

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Davies, Martin, and Jiang Lin. "Nanjing Lianrun Transportation Trade Co., Ltd. v. China Continent Property & Casualty Insurance Co., Ltd. et al." In Chinese Maritime Cases. Springer Berlin Heidelberg, 2021. http://dx.doi.org/10.1007/978-3-662-63239-0_32.

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Davies, Martin, and Jiang Lin. "Yantai Xiangyu Materials Co., Ltd. v. China Continent Property & Casualty Insurance Co., Ltd. Yantai Sub-Branch et al." In Chinese Maritime Cases. Springer Berlin Heidelberg, 2021. http://dx.doi.org/10.1007/978-3-662-63239-0_60.

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Saha, Kshudiram. "Meteorology of the Maritime Continent (Region – III) (Comprising Philippines, Indonesia and Equatorial Western Pacific Ocean)." In Tropical Circulation Systems and Monsoons. Springer Berlin Heidelberg, 2009. http://dx.doi.org/10.1007/978-3-642-03373-5_6.

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Baylis, John. "The Continental Commitment Versus a Maritime Strategy." In British Defence Policy. Palgrave Macmillan UK, 1989. http://dx.doi.org/10.1007/978-1-349-19823-8_2.

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Knecht, Robert W. "Integrated Coastal Zone Management for Developing Maritime Countries." In Coastal Systems and Continental Margins. Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-017-1066-4_2.

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de Goncalves, Franklin O. "Freight Futures and Chartering: A Contingent Claims Analysis Approach applied to Optimal Operational and Investment Decisions in Bulk Shipping." In Current Issues in Maritime Economics. Springer Netherlands, 1993. http://dx.doi.org/10.1007/978-94-015-8153-0_10.

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Bölter, M., and L. Beyer. "Maritime and Continental Antarctic: The Sites of Investigation in Context." In Ecological Studies. Springer Berlin Heidelberg, 2002. http://dx.doi.org/10.1007/978-3-642-56318-8_2.

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Paine, S. C. M. "Japan’s transition from a maritime to a continental security paradigm, 1928–41." In Navies in Multipolar Worlds. Routledge, 2020. http://dx.doi.org/10.4324/9780367855406-7.

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Gonzalez, Rodrigo Milindre, and Sergio Gabriel Caplan. "The Expansion of Argentine Limits in the Continental Shelf: Implications in the International Scope." In Navies and Maritime Policies in the South Atlantic. Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-10600-3_4.

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Holmlund, Joakim, Björn Nilsson, and Johan Rönnby. "Joint Explorations of the Sunken Past: Examples of Maritime Archaeological Collaboration Between Industry and Academia in the Baltic." In Under the Sea: Archaeology and Palaeolandscapes of the Continental Shelf. Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-53160-1_4.

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Conference papers on the topic "Maritime continent"

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Nuryanto, Danang Eko. "A complex empirical orthogonal function for combining two different variables over Indonesian maritime continent." In PROCEEDINGS OF THE 7TH SEAMS UGM INTERNATIONAL CONFERENCE ON MATHEMATICS AND ITS APPLICATIONS 2015: Enhancing the Role of Mathematics in Interdisciplinary Research. AIP Publishing LLC, 2016. http://dx.doi.org/10.1063/1.4940844.

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Ratnawati, H. I., E. Aldrian, and A. H. Soepardjo. "Variability of evaporation-precipitation (E-P) and sea surface salinity (SSS) over Indonesian maritime continent seas." In PROCEEDINGS OF THE 3RD INTERNATIONAL SYMPOSIUM ON CURRENT PROGRESS IN MATHEMATICS AND SCIENCES 2017 (ISCPMS2017). Author(s), 2018. http://dx.doi.org/10.1063/1.5064249.

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Maming, Jumidah, Amrullah Amiruddin, and Reni Andi. "Identification Of Organizational Culture Maritime Continent Based That Affects The Growth And Success Of Small And Medium Enterprises (Smes) In South Sulawesi." In 2nd International Conference on Accounting, Management, and Economics 2017 (ICAME 2017). Atlantis Press, 2017. http://dx.doi.org/10.2991/icame-17.2017.23.

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Chen, H., and T. Moan. "DP Safety for Offshore Drilling and Well Intervention Vessels." In SNAME Maritime Convention. SNAME, 2008. http://dx.doi.org/10.5957/smc-2008-091.

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Barrier method is used to model the safety of dynamic positioning (DP) operation for mobile drilling and well intervention vessels. Two barrier functions are identified which are aimed to prevent loss of position and to prevent loss of well integrity given a loss of position, respectively. The first barrier function is analyzed in this paper. Deficiencies are identified based on the DP incidents on the Norwegian Continental Shelf, and recommendations are proposed to strengthen each barrier element which can improve the safety of DP operations for drilling and well intervention vessels working in the North Sea. The barrier model and recommendations are also valid to DP operations on drilling and well intervention vessels worldwide.
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Reith, Charles A., and Kaj B. Lagstrom. "Reliable Subsea Oil and Gas Transportation Systems." In SNAME 5th World Maritime Technology Conference. SNAME, 2015. http://dx.doi.org/10.5957/wmtc-2015-110.

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This paper is seeking to provide feedback on the use and application of both API-RP-17N &amp; ISO 20815 in subsea field developments and in the progression of floating production system designs by presenting findings and design study recommendations, which are collectively pushing engineering boundaries in the recovery of oil and gas from difficult operational and environmental locations. Lessons Learned, key issues encountered and feed-back are provided from the installation of a subsea facility infrastructure that will deliver gas into the U.K. network from a long distance subsea tieback West of Shetland in the UK Continental Sector and from various FPSO projects and from deep-water FLNG design developments.
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Sanni, Tajudeen. "Refugees and Migrants on the Sea Under African Continental Maritime Regime." In 1st International Conference on Law and Human Rights 2020 (ICLHR 2020). Atlantis Press, 2021. http://dx.doi.org/10.2991/assehr.k.210506.006.

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Awan, M. Saleem, E. Leitgeb, S. Sheikh Muhammad, et al. "Distribution function for continental and maritime fog environments for optical wireless communication." In Digital Signal Processing (CSNDSP). IEEE, 2008. http://dx.doi.org/10.1109/csndsp.2008.4610728.

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Lohan, John, Niall Burke, and Michael Greene. "Climate Variables That Influence the Thermal Performance of Horizontal Collector Ground Source Heat Pumps." In ASME 8th Biennial Conference on Engineering Systems Design and Analysis. ASMEDC, 2006. http://dx.doi.org/10.1115/esda2006-95589.

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The performance characteristics of new heat pumps are usually evaluated under standard test conditions in certified test laboratories prior to their market release. While this data allows potential customers an opportunity to compare different heat pumps under the same conditions it is difficult to assess how variations in operating conditions, particularly around horizontally oriented ground collectors impact on heat pump Coefficient Of Performance (COP). Indeed, harsh winter conditions of continental climates dictate that horizontal collectors are buried sufficiently deep enough to operate in a thermally stable environment, independent of the weather, but this is not as critical in milder maritime climates and shallower collectors that may be influenced by climate are used. This review paper therefore seeks to identify the key climate variables that have been shown to influence the efficiency of horizontal collector heat pump systems. The literature highlights the significant impact of soil moisture content on COP, but the extended relationship between climate, moisture content and COP has not been established. Historical climate data from both a continental and maritime climate is presented and key aspects of their respective weather patterns are compared to assess their capacity to influence soil condition and COP. A series of empirical models linking changes in soil moisture content to fluctuations in soil thermal conductivity, diffusivity and resistance are also presented so that the impact of climate on soil thermal energy content and heat transfer characteristics might be assessed. However, since no one study has experimentally determined the complex relationship between climate, soil heat transfer characteristics and heat pump performance, this paper concludes with an overview of an experimental test facility that allows this relationship to be established for horizontal collector heat pumps in maritime climates.
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Halsne, Marita, Narve Oma, Gerhard Ersdal, et al. "In Service Experiences With Ship-Shaped Floating Production Units." In ASME 2020 39th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2020. http://dx.doi.org/10.1115/omae2020-19287.

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Abstract FPSOs and FSOs have been used on the Norwegian continental shelf for petroleum production, storage and offloading since the 1980’s and have been increasingly common since the end of the 1990’s. During these years a significant amount of experience has been gathered. On the Norwegian Continental Shelf (NCS) shipowners and operators are obliged to report damages and incidents to the Petroleum Safety Authority Norway (PSA). This article gives an overview of reported incidents related to the structural and maritime systems on offshore ship shaped units in the petroleum activity (FPSOs and FSOs) on the Norwegian Continental Shelf. Reported incidents are summarised with a focus on the period 2000 to 2019. The incidents include cracks, dents, corrosion, turret incidents, green water, position keeping systems, stability and ballasting, collisions and incidents related to the offloading systems as reported by operators and shipowners to the PSA. A summary of the reported damages and incidents are discussed with respect to common causes based on available data. The importance and the possible consequences of such incidents are further discussed.
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Kvitrud, Arne, Gerhard Ersdal, and Jan-Erik Vinnem. "Risk Indicators for Major Accidents on Load Bearing Structures and Maritime Systems in the Petroleum Industry." In ASME 2008 27th International Conference on Offshore Mechanics and Arctic Engineering. ASMEDC, 2008. http://dx.doi.org/10.1115/omae2008-57095.

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To monitor the development of the risk of major accidents of structures and maritime systems on the Norwegian Continental Shelf a set of incident indicators has been established. These indicators are given a weight related to the fatality risk predictions in order to develop a total risk indicator. Aggregated and weighted indicators as well as individual indicators are presented and evaluated. In addition indicators related to barriers are established giving a method to monitor the performance as a function of time, and to benchmark the participants in the industry. The present paper describes the method used in the risk level project to monitor the risk related with emphasis on structures and maritime systems, including hazards as wave in deck, vessel collisions and cracks on the structures. The paper further presents the actual development using the methodology, and the identified major contributors to the risk level.
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Reports on the topic "Maritime continent"

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Jordan, Frank E., and III. A Strategic Approach to the Maritime-Continental Strategy Debate. Defense Technical Information Center, 1987. http://dx.doi.org/10.21236/ada436918.

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Atkinson, Dan, and Alex Hale, eds. From Source to Sea: ScARF Marine and Maritime Panel Report. Society of Antiquaries of Scotland, 2012. http://dx.doi.org/10.9750/scarf.09.2012.126.

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The main recommendations of the panel report can be summarised under four headings: 1. From Source to Sea: River systems, from their source to the sea and beyond, should form the focus for research projects, allowing the integration of all archaeological work carried out along their course. Future research should take a holistic view of the marine and maritime historic environment, from inland lakes that feed freshwater river routes, to tidal estuaries and out to the open sea. This view of the landscape/seascape encompasses a very broad range of archaeology and enables connections to be made without the restrictions of geographical or political boundaries. Research strategies, programmes From Source to Sea: ScARF Marine and Maritime Panel Report iii and projects can adopt this approach at multiple levels; from national to site-specific, with the aim of remaining holistic and cross-cutting. 2. Submerged Landscapes: The rising research profile of submerged landscapes has recently been embodied into a European Cooperation in Science and Technology (COST) Action; Submerged Prehistoric Archaeology and Landscapes of the Continental Shelf (SPLASHCOS), with exciting proposals for future research. Future work needs to be integrated with wider initiatives such as this on an international scale. Recent projects have begun to demonstrate the research potential for submerged landscapes in and beyond Scotland, as well as the need to collaborate with industrial partners, in order that commercially-created datasets can be accessed and used. More data is required in order to fully model the changing coastline around Scotland and develop predictive models of site survival. Such work is crucial to understanding life in early prehistoric Scotland, and how the earliest communities responded to a changing environment. 3. Marine &amp; Maritime Historic Landscapes: Scotland’s coastal and intertidal zones and maritime hinterland encompass in-shore islands, trans-continental shipping lanes, ports and harbours, and transport infrastructure to intertidal fish-traps, and define understanding and conceptualisation of the liminal zone between the land and the sea. Due to the pervasive nature of the Marine and Maritime historic landscape, a holistic approach should be taken that incorporates evidence from a variety of sources including commercial and research archaeology, local and national societies, off-shore and onshore commercial development; and including studies derived from, but not limited to history, ethnology, cultural studies, folklore and architecture and involving a wide range of recording techniques ranging from photography, laser imaging, and sonar survey through to more orthodox drawn survey and excavation. 4. Collaboration: As is implicit in all the above, multi-disciplinary, collaborative, and cross-sector approaches are essential in order to ensure the capacity to meet the research challenges of the marine and maritime historic environment. There is a need for collaboration across the heritage sector and beyond, into specific areas of industry, science and the arts. Methods of communication amongst the constituent research individuals, institutions and networks should be developed, and dissemination of research results promoted. The formation of research communities, especially virtual centres of excellence, should be encouraged in order to build capacity.
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Rutledge, Steven, Wie-Kuo Tao, Toshihisa Matsui, and Brenda Dolan. Investigation of Hydrometeor Distributions in Continental and Maritime Storm Systems: Application of Cloud-Resolving Simulations, a Polarimetric Scanning Radar Simulator and Polarimetric Radar Observations. Office of Scientific and Technical Information (OSTI), 2019. http://dx.doi.org/10.2172/1571168.

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