scholarly journals Typology of The Coastal Countryside in Supporting Development of North Coast Region in West Java

2020 ◽  
Vol 22 (4) ◽  
pp. 486-496
Author(s):  
Apriadi Budi Raharja ◽  
Supratognyo Aji ◽  
Deden Syarifudin
Keyword(s):  
Rural Communities ◽  
Rapid Development ◽  
Characteristic Parameter ◽  
Industrial Area ◽  
North Coast ◽  
Northern Coast ◽  
West Java ◽  
Fish Catch ◽  
Rural Typology ◽  
Area North

The pressure from rapid development causes condition of resources and living quality to be less than ideal for future development. The economic characteristics of northern coast regions of West Java commonly deals with fish farm, ground fish catch, industrial area, ship repair, and tourist. This study aimed to reveal the typology of rural area, north coast of West Java province. The analysis used was multivariate to identify a group of objects that have the semblance of a characteristic parameter based on natural resources and human resources. Research locus on six counties that consist of 124 identified villages is a village along northern coast of West Java. Based on analysis of rural typology, four of the rural types were found, namely; typology 1 (comprised 55 villages); typology 2 (48 villages); typology 3 (10 villages); typology 4 (11 villages). Coastal villages of Pantura have a fast transition, However the transition occurred tends to shape village’s characteristic and still unable to improve service quality and quality of life of rural communities.

scholarly journals Studi Perubahan Garis Pantai Berdasarkan Interpretasi Citra Satelit Landsat dan Perhitungan Rasio Lahan di Wilayah Pesisir Indramayu Jawa Barat

2018 ◽  
Vol 1 (1) ◽  
Author(s):  
Thonas Indra Maryanto ◽  
Wiwin Windupranata ◽  
Samsul Bachri
Keyword(s):  
Satellite Image ◽  
Image Data ◽  
North Coast ◽  
Transitional Region ◽  
Northern Coast ◽  
Residential Areas ◽  
West Java ◽  
The North ◽  
Average Sedimentation Rate ◽  
Landsat Satellite

ABSTRAKWilayah pesisir sebagai kawasan peralihan yang menghubungkan ekosistem darat dan ekosistem laut, sangat rentan terhadap kerusakan dan perubahan yang diakibatkan oleh berbagai aktifitas manusia di darat maupun di laut. Kabupaten Indramayu merupakan salah satu wilayah di Pesisir Utara Jawa Barat yang mengalami kerusakan paling parah diantara seluruh kabupaten di wilayah pesisir Utara Jawa Barat serta memiliki penggunaan lahan pesisir yang cukup lengkap mulai dari pemukiman, persawahan, tambak, dan industri (PLTU dan MIGAS)..Besarnya perubahan garis pantai yang meliputi abrasi dan sedimentasi diturunkan dari data citra satelit Landsat wilayah pesisir Kabupaten Indramayu tahun 1994-2009 dengan metode komposit RGB 4, 5, 7 dan Metode AGSO kemudian dilakukan proses digitasi.. Luas abrasi di 11 Kecamatan Pesisir Indramayu dari tahun 1994 – 2009 sebesar 3900,41 Ha dengan laju abrasi rata-rata sebesar 23,64 Ha/ tahun dan Luas sedimentasi sebesar 650,29 Ha dengan laju sedimentasi rata-rata sebesar 4,81 Ha/tahun. Hasil perhitungan regresi terhadap rasio lahan penduduk untuk tahun 2015 sebesar 0,07 Ha/ jiwa dan menurun pada tahun 2025 menjadi 0,05 Ha/jiwa .Rasio lahan petani untuk tahun 2015 sebesar 0,66 Ha/petani dan menurun menjadi 0,55 Ha/petani di tahun 2025.Kata Kunci : Pesisir indramayu, citra satelit, abrasi dan sedimentasi, Rasio lahanABSTRACTCoastal areas as a transitional region connecting the land ecosystems and marine ecosystems, are vulnerable to damage and changes caused by various human activities on land and at sea. Indramayu regency is one of the areas in the North Coast of West Java is the most severely damaged among all districts in the northern coast of West Java and has a coastal land use complete enough from residential areas, wet rice fields, ponds, and industrial (power plant and Gas). The number of change in coastal line include erosion and sedimentation derived from Landsat satellite image data coastal areas of Indramayu district in 1994-2009 with the composite method RGB 4, 5, 7 and methods AGSO then do the digitization process. The extent of abrasion in 11 districts of the coastal Indramayu from 1994 - 2009 are 3900.41 hectares with average abrasion rate of 23.64 ha / year and sedimentation area of 650.29 hectares with an average sedimentation rate of 4.81 ha / year. Results of regression calculations to land ratio for the 2015 population of 0.07 ha / life and decreased in 2025 to 0.05 hectares /life .Rasio farmers' fields for 2015 of 0.66 ha / farmer and decreased to 0.55 Ha / farmers in 2025. Keywords: Coastal area of indramayu, satellite imagery, erosion and sedimentation, land Ratio

scholarly journals Preliminary results of drift-bottle releases and recoveries in the Western Tropical Atlantic

1967 ◽  
Vol 16 (1) ◽  
pp. 13-22 ◽  
Author(s):  
Ellen F. Luedemann
Keyword(s):  
Surface Current ◽  
Northeastern Brazil ◽  
Brazilian Coast ◽  
Northern Coast ◽  
The North ◽  
Strong Current ◽  
North Brazil ◽  
Equatorial Current ◽  
The Caribbean ◽  
Area North

In February-March 1963, during the Equalant Operation for the ICITA program, 476 drift-bottles were released at the equatorial waters off the northern Brazilian coast (01ºS to 09ºN and 043ºW to 053ºW). Thirty-five, bottles were recovered (7,4%). Those were classed in five groups according to their different velocity ranges and areas of recovery (Trinidad Island; Lesser Antilles; Caribbean and Florida area; north Brazil; northeastern Brazil). The recoveries of bottles released within 300 nm off the northern and northeastern coast of Brazil confirmed a strong current along the north and northeast coast in northwestern direction (South Equatorial Current and branches). In late February-early March the bottles showed maximum velocities of this current (3,6 knots). The region off the northern coast of Brazil, between 05ºN and 09ºN up to 050ºW seems to have been under the influence of an eastward component of the surface current in this same period, while at late March this influence appears to have been weaker. In the region from Trinidad Island to Yucatan Peninsula the current seems to be stronger on the northeastern side of the Caribbean Sea.

scholarly journals PESANTREN SALAF: PERUBAHAN SOSIAL DAN SUBLIMASI IDENTITAS DENGAN KOMBINASI TASAWUF, FIQIH DAN TAUHID (Model Pesantren di Kabupaten Tasikmalaya Jawa Barat)

2020 ◽  
Vol 4 (2) ◽  
pp. 87-105
Author(s):  
Muhammad Solahudin ◽  
Ecep Ismail ◽  
Irwan Abdurrohman
Keyword(s):  
Social Change ◽  
School Environment ◽  
Max Weber ◽  
Rapid Development ◽  
Boarding School ◽  
Theory Of Action ◽  
West Java ◽  
Cultural Elements ◽  
The Times ◽  
The One

On the one hand, in the environment of the Pesantren salaf community, a kind of environment and tradition is formed which shows its unique, even unique characteristics, which are only understood by the community. Gus Dur, in this case, stated that the Pesantren salaf community is a community that has its own subcultural in the middle of society with the complexity of the problems in it. But on the other hand, there is a very rapid development of science and technology, so it demands pesantren salaf to make changes to adjust to the times, both in terms of the education system, the boarding school environment, institutions, leadership patterns, and others. Therefore, the study contained in the title "Pesantren Salaf: Social Change and Sublimation of Identity (Pesantren Model in West Java)", is very important to be carried out.The purpose of this study is none other than to find the concept of changes that occur in Pesantren salaf in West Java. For more details, they are: 1) uncovering the factors that drive changes in pesantren in West Java; 2) reveal pesantren's efforts in facing the challenges of the times, and 3) find forms of changes that occur in the Pesantren salaf in West Java.This research departs from a thought that social change will occur due to four things. First, Evolution. This theory states that humans as part of a cultured society will naturally develop gradually from simple forms to complex and perfect stages. Second, Conflict. This theory strongly believes that change will only occur if there is conflict. Third. Functional Theory. Social change occurs because of the disharmony between cultural elements. Fourth, Cycle Theory. Social change by itself will occur and cannot be controlled.The method used in this research is descriptive. In the process, the data is collected and compiled. After the data is collected and arranged in such a way, the authors analyze it and provide interpretation, with a qualitative approach. So that it is expected to be able to uncover the realities of the Pesantren salaf which are changing in the community.The results of the study stated that the Pesantren salaf can adapt well to social change by bringing up certain identities. This shift in identity needs to be examined and studied through the theory of action put forward by Max Weber. First, zweckrational. This theory is known as rational-purpose. In doing something always with a good and accurate calculation. Second, wertrational or rational-values. The involvement of the subject is directly involved in matters of absolute importance. The four traditionalists. This theory of action rests on established and established customs or traditions. Traditionalist theories respect existing authority.

scholarly journals Spatial Analysis of Coastline Change by Remote Sensing in the North Coast of Karawang Regency

2020 ◽  
Vol 3 (2) ◽  
Author(s):  
Roberto Pasaribu ◽  
Firman Agus H. ◽  
Liliek Soeprijadi
Keyword(s):  
Shoreline Change ◽  
Rate Of Change ◽  
North Coast ◽  
Landsat 8 ◽  
Northern Coast ◽  
Shoreline Changes ◽  
The Road ◽  
Coastline Change ◽  
The North ◽  
Landsat 7

<p><em>The existence of the coast in the northern part of Karawang Regency is very worrying. Seawater<strong> </strong>that was far up to tens of meters from the side of the road, is now on the lip of the road, even some parts of the road are cut off due to abrasion of seawater. Some villages were affected by abrasion erosion. One of the effects of damage due to abrasion and sedimentation is the occurrence of shoreline changes. This change in coastline will affect people's lives and spatial planning for the development of the area. For this reason, this study aims to determine the extent and rate of shoreline changes that occurred on the coast of Karawang Regency in the periods of 1989, 1995, 2001, 2005, 2009, 2016, and 2018. The shoreline data was obtained from the extraction of Landsat 3 MSS, Landsat 5 TM, Landsat 7 ETM +, and Landsat 8 </em><em>OLI</em>-<em>TIRS after the NDWI process was previously carried out. While the rate of change is calculated at 6 sample point locations scattered along the northern coast of Karawang Regency. The results showed that the largest area damaged by abrasion occurred in Sedari Village covering an area of 166.802 hectares, and the area formed by the largest sedimentation occurred in Muara Cilamaya Village at 276,318 hectares. Meanwhile, the fastest rate of shoreline change due to abrasion occurred in Sukajaya Village at 10 meters </em>/<em>year, while the slowest in Sedari Village at 3.77 meters / year. The fastest sedimentation process in Muara Cimalaya Village is 4.5 meters / year, while the late one in Tanjung Pakis Village is 3.09 meters / year.</em><em></em></p><p><strong><em>Keywords: </em></strong><em>Abra</em><em>sion, Accretion, Coastline Changes, Karawang</em><em></em></p>

scholarly journals Climate change and Canada’s north coast: research trends, progress, and future directions

2018 ◽  
Vol 26 (1) ◽  
pp. 82-92 ◽  
Author(s):  
James D. Ford ◽  
Nicole Couture ◽  
Trevor Bell ◽  
Dylan G. Clark
Keyword(s):  
Climate Change ◽  
Current Knowledge ◽  
Geographic Location ◽  
Climate Change Impacts ◽  
Evidence Base ◽  
North Coast ◽  
Future Research ◽  
Northern Coast ◽  
Knowledge Mobilization ◽  
Interdisciplinary Approaches

This paper identifies and characterizes current knowledge on climate change impacts, adaptation, and vulnerability for Canada’s northern coastline, outlining key research gaps. Warming temperatures and increased precipitation have been documented across the northern coast, with the rate of sea ice decline ranging from 2.9% to 10.4% per decade. Storm intensity and frequency is increasing, and permafrost is warming across the region. Many of these changes are projected to accelerate in the future, with in excess of 8 °C warming in winter possible under a high-emission scenario by 2081–2100. Vulnerability to these changes differs by region and community, a function of geographic location, nature of climate change impacts, and human factors. Capacity to manage climate change is high in some sectors, such as subsistence harvesting, but is being undermined by long-term societal changes. In other sectors, such as infrastructure and transportation, limitations in climate risk management capacity result in continuing high vulnerabilities. There is evidence that adaptation is taking place in response to experienced and projected impacts, although readiness for adaptation is challenged by limited resources, institutional capacity, and a need for support for adaptation across levels of government. Priority areas for future research include (i) expanding the sectoral and geographic focus of understanding on climate change impacts, adaptation, and vulnerability; (ii) integrating climatic and socio-economic projections into vulnerability and adaptation assessments; (iii) developing an evidence base on adaptation options; and (iv) monitoring and evaluating the effectiveness of adaptation support. Cross-cutting themes for advancing climate change impacts, adaptation, and vulnerability research on the north coast more broadly include the need for greater emphasis on interdisciplinary approaches and cross-cultural collaborations, support for decision-orientated research, and focus on effective knowledge mobilization.

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