Relevant bibliographies by topics / Continent maritime

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  1. Journal articles

Academic literature on the topic 'Continent maritime'

Author: Grafiati
Published: 4 June 2021
Last updated: 19 February 2022

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Journal articles on the topic "Continent maritime"

1

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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2

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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3

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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4

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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5

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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6

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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7

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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8

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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9

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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10

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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