Rising Sea Water Research Articles

Utilization of Muria Strait Toponymy data in mitigation: Building resilience to disaster risk

Abstract The North Coast of Java Island, including the area around Kendal to Rembang (formerly known as the Muria Strait region), is susceptible to sea water rise and land subsidence, which pose a significant risk to the lives of its inhabitants. Similarly, the districts of Demak, Kudus, Pati, Rembang, and Juwana are also vulnerable to these threats given that they were formed by alluvial deposits and are now densely populated. However, the community’s resilience to various changes in Muria Strait’s geosphere can be observed in the development of local knowledge, including toponymy. In the modern era, toponymic data can be used as instruments to support disaster mitigation and recovery efforts. The information content obtained after the toponymy study can be used as an instrument to increase public awareness and develop a targeted mitigation infrastructure. Given the community’s vulnerability to a range of disasters exacerbated by climate change, the objective of this research is to disseminate the findings of a toponym study of the Muria Strait, with a focus on the potential of these data to inform disaster-mitigation strategies. Toponymy data analysis was conducted using an ethnopedological approach in the context of archaeological and historical research. This approach was also necessary to analyse historical sources related to soil cover/land use (SLC) and changes in the geosphere of the Muria Strait over time.

ANALYZING THE CAUSE OF TIDAL FLOODING IN RANDUSANGA KULON VILLAGE, BREBES DISTRICT, BREBES REGENCY

In Indonesia, many regions experienced inundation as a result of the rise of seawater. One of them is the coast of Randusanga Kulon village. The coastal area of Randusanga Kulon village has recreation spots and ponds. These areas are located at the edge of a river estuary which is directly adjacent to the sea. On the other hand, the settlement area is located just 3 km from the seaside. Therefore, when a high tide occurs, the recreation, pond, and settlement areas will be hit by tidal floods. This study aimed to analyze the causes and impacts of tidal floods that hit Randusanga Kulon Village of Brebes District of Brebes Regency.The methods used to process the data are the Formzahl and Admiralty methods. The result of calculating using the admiralty method is that Brebes Sea has Mixed Semi-Diurnal type of daily tides with a Formzahl value of 0,9948. The value of HHWL was calculated to determine the prediction of seawater rise. By using the Admiralty Method the result is 47 cm, and by using SLR data due to global warming, it is 30 cm.

What if the upwelling weakens? Effects of rising temperature and nutrient depletion on coastal assemblages

Surface temperature of the oceans has increased globally over the past decades. In coastal areas influenced by eastern boundary upwelling systems (EBUS), winds push seawater offshore and deep, cold and nutrient-rich seawater rise towards the surface, partially buffering global warming. On the North coast of Portugal, the NW Iberian upwelling system allows extensive kelp forests to thrive in these “boreal-like” conditions, fostering highly diverse and productive communities. However, the warming of the upper layer of the ocean may weaken this upwelling, leading to higher sea surface temperature and lower nutrient input in the coastal areas. The effects of these changes on the structure and function of coastal ecosystems remain unexplored. The present study aimed to examine the combined effects of elevated temperature and nutrient depletion on semi-naturally structured assemblages. The eco-physiological responses investigated included growth, chlorophyll fluorescence and metabolic rates at the levels of individual species and whole assemblages. Our findings showed interactive effects of the combination of elevated temperature with nutrient depletion on the large canopy-forming species (i.e., kelp). As main contributor to community response, those effects drove the whole assemblage responses to significant losses in productivity levels. We also found an additive effect of elevated temperature and reduced nutrients on sub-canopy species (i.e., Chondrus crispus), while turfs were only affected by temperature. Our results suggest that under weakening upwelling scenarios, the ability of the macroalgal assemblages to maintain high productivity rates could be seriously affected and predict a shift in community composition with the loss of marine forests.

Enterococci pathways to coastal waters and implications of sea level rise

Highly urban coastal communities in low lying areas and with high water tables are vulnerable to sea-level rise and to corresponding increases in coastal groundwater levels. Stormwater conveyance systems are under increased risk. Rising groundwater levels affect the hydraulics of the stormwater system thereby increasing contaminant transport, for example the fecal indicator bacteria enterococci, to coastal waters. This study offers a unique opportunity to evaluate the impacts of increased contaminant transport on marine coastal environments. Here we assessed historic and recent coastal water quality, stormwater sampling data, groundwater monitoring and tidal elevations near the coastline, in the context of altered hydraulics within the system. Two pathways of enterococci to marine waters were identified. Direct discharge of contaminated stormwater runoff via the stormwater outfalls and tidally driven contaminated groundwater discharge. As sea level continues to rise, we hypothesize that a diminished unsaturated zone coupled with altered hydraulic conditions at the coastal groundwater zone will facilitate the transport of enterococci from urban sediments to the study site (Park View Waterway in Miami Beach, FL USA). We recommend improvements to the stormwater conveyance system, and maintenance of the sanitary sewer system to mitigate these impacts and minimize transport of enterococci, and other stormwater pollutants to coastal waters. The results of this study can be useful to interpret high enterococci levels in low lying coastal areas where groundwater is influenced by rising sea water levels.

Architecture of Oxfordian coral buildups along the Atlantic margin of Morocco

Oxfordian (Upper Jurassic) coral buildups developed widely in Tethys and Atlantic realms, during a time when paleoclimate potentially swung between greenhouse climate and cold snaps. Buildups were constructed by platy and branching corals, sponges and microbialites. Although their initiation is commonly linked to the Upper Jurassic global transgression, a number of global and local factors may have influenced buildup growth and demise (e.g. climate, shelf geometry, detrital input). Extensive outcrops of Oxfordian buildups in Morocco provide an opportunity to investigate the relationship between external drivers and buildup fauna and architecture. Here we show that the interplay of local accommodation changes, rising sea water temperature, and increasing pCO2 linked to the onset of the Middle Oxfordian global transgression were the main drivers for buildup initiation, which was synchronous across the basin. The demise of the coral buildups in Morocco was linked to a regression, dated no later than Upper Oxfordian, the establishment of partly evaporitic conditions across the basin, and to localized influx of coarse-grained siliciclastics, the latter likely driven by synsedimentary tectonic activity. Serial logged sections, outcrop panoramas and detailed facies analysis show that low-relief deeper-water buildups of Dimorpharaea platy corals evolved into higher-relief diversified buildups where shallower-water reworking produced coral rubble and large clinoforms. Buildup diachronicity is apparent, with younger coral bioherms growing in the depressions created between the initial bioherms. Size of buildups ranges from 2 m wide and 0.5 m thick, to 700 m wide and 80 m thick. The outcrops provide constraints on geobody architecture and heterogeneity in the subsurface of Morocco and North America, where facies-controlled dolomitization of high-energy buildup and clinoform facies is a main driver for porosity development.

Saltwater Intrusion and Agricultural Land Use Change in Nga Nam, Soc Trang, Vietnam

Under the effects of saltwater intrusion from rising sea water levels, climate change, and socioeconomic issues, the Nga Nam district in Vietnam has suffered damage to its agriculture and changes in agricultural land use. This study aimed to investigate the factors that influenced land use changes and to propose approaches to limit the changes in agricultural land use. The damage caused by saltwater intrusion on agricultural production was evaluated via the use of secondary data collected from the Department of Infrastructure Economics of the Nga Nam district in the period of 2010–2021. The results show that during the 2010–2015 period, agricultural production areas were affected in 2010, 2012, and 2015. In the period of 2015–2021, the trend of saltwater intrusion along the damaged area remarkably decreased due to the work of saltwater-preventing structures. In this period, the area of annual plants increased, while that of fruit trees decreased. In the area comprising annual plants, the area using the triple rice land use type converted into an area using the double rice and double rice–fish ones. Lands for fruit trees transitioned from mixed farming to specialized farming to raise the economic efficiency for farmers. These changes were affected by four main factors: the physical factor, the economy, society, and the environment. The environmental and economic factors were seen to play the most important role as drivers of changes in land use. The factors of saltwater intrusion and acid-sulfate-contaminated soil, consumer markets, floods, drought, profit, and investments were noted to be significant drivers in agricultural land use change. Thus, both structural and non-structural approaches are suggested to inhibit the safeguard changes in the future.

The thermophilic sea anemone Telmatactis cricoides (Cnidaria, Hexacorallia) in the western Mediterranean: filling gaps in the knowledge of the distribution

Abstract Several individuals of the sea anemone Telmatactis cricoides (Duchassaing, 1850) (order Actiniaria) were observed in the Mediterranean continental Spanish coast (Almeria) and the Balearic Islands (Mallorca) showing an expansion of the species, possibly related to rising sea water temperatures. This finding contributes to increase the knowledge on the geographical distribution range of this actiniarian in the Mediterranean basin.

Influence of Anomalous Upwelling on the Water Mass of South Java during Two Positive Indian Ocean Dipole in 2015 and 2019

Upwelling is a phenomenon that often occurs in the ocean. Upwelling can be interpreted as the process of rising sea water masses from below the surface to the surface due to the vacancy of sea water masses at the surface. The upwelling phenomenon will cause many anomalies that have a direct impact on ocean dynamics, one of which is the dynamics that occur in the waters south of Java. The formation of the coastal upwelling phenomenon in the waters south of Java in 2015 and 2019 was the cause of the active Positive IOD in both years. By carrying out time series analysis and spatial data visualization processes as well as correlation methods to determine the relationship between parameters, this research aims to discuss and find out about the influence of coastal upwelling dynamics on the waters of southern Java in 2015 and 2019. The results obtained from this research show that the coastal upwelling phenomenon formed in 2015 and 2019 along the waters of southern Java resulted anomalies in dynamic patterns in the form of decreasing sea surface temperatures and increasing chlorophyll-a concentrations

APPLICATION OF SMOOTHED PARTICLE HYDRODYNAMICS ON A LOW LEVEL QUAY DECK

Rising sea water level projections challenge the existing levels within ports. Although air gaps have been a traditional means to avoid a fight with the force of the sea, such principle cannot be implemented easily in existing ports, or even for new projects, since these projects require interfacing with their surroundings. More and more, the interaction between the sea (and in particular extreme wave climates) and existing low quay deck levels for open types of quay walls has to be estimated. Apart from relying on physical model testing, the numerical world comes to our rescue. Significant advances have been made over the past decennium with the practical commercial implementation of smoothed particle hydrodynamics for practical engineering problems. This article describes a practical example of such an assessment for a particular project in the port of Ostend, Belgium.

Water Management to Cope with the Effects of Climate Change Best practices in Water Management at Wageningen University & Research

Wageningen University & Research studies the causes of heavy rainfall and droughts and is looking for solutions to these phenomena [1]. For example, green spaces in the urban environment ensure that water can be drained into the ground. Storage of water is also important, because not only the number of heavy rains is increasing, also there are longer periods of drought. On WUR Campus, these principles of coping with flooding and drought are applied. There is a sizeable area of green space which serves as a groundwater discharge area. The large ponds on campus are used to collect and store excess surface water. During droughts the ponds retain water on campus. In two campus buildings, rain is harvested for flushing toilets and watering inner gardens. The rainwater is harvested from rooftops and stored in underground water tanks. A natural garden was laid out in 1998, and four years ago a natural wetland garden was added to the campus.The effects of climate change, such as droughts and rising sea water levels affect freshwater supplies, which makes efficient use of water increasingly important. WUR aims to reduce consumption of tap water every year, by increasing water use efficiency and switching to sources other than tap water.

Literature Study on Conditions of Sea Surface Temperature and Seawater Rise in Indonesia Detected by Remote Sensing

The Sea Surface Temperature (SST) is an important parameter for climate dynamic issues either globally or regionally as well as for global warming issues. In some condition the parameter can cause melting glaciers that will influence the rise of the sea levels. The further effect will be the climate change with the weather phenomena such as storms, hurricanes and heavy rains. As the result, the changes of the planting seasons occur and all of these will harm human life on earth. If there is no prevention with the condition of the parameter it is predicted that by 2040 the sea levels will rise highly because of the melting polar ice caps that will cause the sink of theislands. The SST has been detecting using remote sensing methods for 32 years in Indonesia. The trend has increased to reduce the damage of infrastructure and the activity disturbance of coastal communities. Indonesian country optimistically commits to achieve the target of net zero emission by 2060. The Indonesian government has stated nationally the climate target commitments determined for Indonesia and will strive to maintain the main target of reducing greenhouse gas emission into 41% by 2030.

Fresh Water availability and Its Global challenge

Water is prime natural resources fulfilling our needs in a precisious assets.we must acts to preserve and utilize every drop of water.water resources can be assessed on the basis of surface and subsurface water bodies.Climate change impact on ground Water the impact of climate change on ground water has been studied much less than the impact on surface waters. Ground water reacts to climate change mainly due to change in ground water recharge,but also change in river level in response to increase in mean Temperature,precipitation ,variability and sea level as mean precipitations.Changing land use pattern due to increasing ,urbanization, industrialization and agriculture activities are serious issues that causing increase ground water with drawal resulting in depletion of ground water resources and mining of ground water resources,along with deterioration of water quality.Rainfall is highly irregular and erratic and declining year to year due to change climatic conditions as result of serious deforestation global warming etc.Human health is affected by change in biodiversity and ecosystem.Climate change will affect the quality of drinking water and impact of fresh water availability and impact on public health. About 70% of Earth’s surface is water of which 97.5% is salty water and 2.5% is fresh water. Less than 1% of this 2.5% amount of freshwater is accessible. As sea water rise’s , salt water of ocean in filtrate as coastal fresh water due heavy rainfall and flooding waste more fertilizer and municipal sewage mixed with costal fresh water and change alter into more oxygen dead zone. Weather extreme and climate variability is main driver of food production in recent global challenge. Recent global challenge food security, fresh water availability, increase incidence of extreme high sea level. Loss of agriculture reproduction and increase in food prices and changes in weather patterns and alter availability and quality of water in many part of world. Climate change is an on-going phenomenon. This will inevitably bring about numerous environmental problems, including alterations to the hydrological cycle, which is already heavily influenced by anthropogenic activity.Chemical fertlizer’s has been adversely affecting the flora, fauna as well as soil quality . more ever every year plant pathogen are causing loss of 10 to 20% of agricultural production worldwide. Ground water will be vital to alleviate some of the worst drought situations. flooding and contaiminated water supplies, more intense weather events are likely to increase to risk of infectious disease epidemics and erosion of low-lying and costal land. Climate Chang will affect the quality of drinking Water and impact of fresh water availlablity and impact on public health it’s better to use UV Water purifiers.This paper will explore what climate change. Water is prime natural resources fulfilling our needs in a precisious assets.we must acts to preserve and utilize every drop of water.water resources can be assessed on the basis of surface and subsurface water bodies.Climate change imapact on ground Water the impact of climate change on ground water has been studied much less than the impact on surface waters. Ground water reacts to climate change mainly due to change in ground water recharge,but also change in river level in response to increase in mean Temperature,precipitation ,variability and sea level as mean precipitations.Changing land use pattern due to increasing ,urbanization, industrialization and agriculture activities are serious issues that causing increase ground water with drawal resulting in depletion of ground water resources and mining of ground water resources,along with deterioration of water quality.Rainfall is highly irregular and erratic and declining year to year due to change climatic conditions as result of serious global warming .Impacts of sea level rise on salinity intrusion global climate change has resulted in gradual sea level rise. sea level rise can cause saline water to migrate up stream in estuaries and rivers,thereby threating fresh water habitat and drinking- water supplies.Hydrology all the costal margin; fresh ground water flowing in land areas meets with saline ground water from the ocean. the fresh ground water flows from in land areas towards the coast where elevation and groundwater level are lower because salt water has higher content of dissolved salt and minerals. it denser the fresh water,causing it to have hydraulic head than freshwater. hydraulic head refers to the liquid pressure exerted by water column. the higher pressure density of salt water causes it to move into costal aquifiers in a a wedge shape under the freshwater. the salt water and fresh water meets in a transition zone where mixing occurs through dispersion and diffusion.

Coastal Erosion and The Minas Bay: An Analysis

Located on the Bay of Fundy, the Joggins Fossil Cliffs are lined with fifteen kilometres of exposed rock layers that hold relics of 300 million years (ENSECO, 2023). Characterized by extreme tides, turbulent currents, silt-laden waters, and a soft substrate, it is here that 100 billion tons of seawater rise and fall as much as 48 feet every day. Research indicates that erosion rates are expediting and dramatic tides are not stalling these processes. Erosion instigated by water processes is destructive, causing environmental degradation and posing threats to crops, pastures, and forests. However, under these conditions, the first definition of rare organisms preserved in their original ecological context, are under threat. Founders of modern geology, Charles Lyell and William Dawson, discovered tetrapods, amphibians, and reptiles, preserved in the upright fossilized trees (ENSECO, 2023). ArcGIS Pro and photogrammetry techniques have been used to georeference and transpose aerial photography and satellite imagery onto a digital elevation model (DEM). My hypothesis is that erosion rates have been increasing over time due to extreme climate events that have expedited environmental variables. The results of this research will indicate if changes in climate are leading to the escalation of erosion in this area. This is significant to determine how long we might have before this incredible archive of biological material is no longer available.

Environmental Statistical Analysis on the Impacts of Marine Mucilage on some Seawater Quality Parameters

Marine mucilage creates significant pollution in seawater due to the high amounts of nitrogen and phosphorus discharges. The water quality of the Sea of Marmara has been damaged due to this environmental problem with the rising sea water temperature since 2020. This study aims to investigate the statistical differences in the impact of marine mucilage in the Sea of Marmara between 2020 and 2021, taking into account dissolved oxygen, pH, seawater, and ambient temperature. Ten sampling locations were established for this purpose on the Anatolian part of the Sea of Marmara. The statistical analysis revealed there is a statistically significant difference with a percent of 99 confidence levels at all sampling points. The variables pH and dissolved oxygen revealed a difference between 2020 and 2021, however, no statistically significant results were determined for the seawater temperature.

Fresh Water availability and It’s Global challenge

Water is prime natural resources fulfilling our needs in a precisious assets. We must acts to preserve and utilize every drop of water. Water resources can be assessed on the basis of surface and subsurface water bodies. Climate change impact on ground Water the impact of climate change on ground water has been studied much less than the impact on surface waters. Ground water reacts to climate change mainly due to change in ground water recharge, but also change in river level in response to increase in mean Temperature, precipitation ,variability and sea level as mean precipitations. Changing land use pattern due to increasing, urbanization, industrialization and agriculture activities are serious issues that causing increase ground water with drawal resulting in depletion of ground water resources and mining of ground water resources, along with deterioration of water quality. Rainfall is highly irregular and erratic and declining year to year due to change climatic conditions as result of serious deforestation global warming etc. Human health is affected by change in biodiversity and ecosystem. Climate change will affect the quality of drinking water and impact of fresh water availability and impact on public health. About 70% of Earth’s surface is water of which 97.5% is salty water and 2.5% is fresh water. Less than 1% of this 2.5% amount of freshwater is accessible. As sea water rise’s, salt water of ocean in filtrate as coastal fresh water due heavy rainfall and flooding waste more fertilizer and municipal sewage mixed with coastal fresh water and change alter into more oxygen dead zone. Weather extreme and climate variability is main driver of food production in recent global challenge. Recent global challenge food security, fresh water availability, increase incidence of extreme high sea level. Loss of agriculture reproduction and increase in food prices and changes in weather patterns and alter availability and quality of water in many part of world. Climate change is an on-going phenomenon. This will inevitably bring about numerous environmental problems, including alterations to the hydrological cycle, which is already heavily influenced by anthropogenic activity. Chemical fertlizer’s has been adversely affecting the flora, fauna as well as soil quality . more ever every year plant pathogen are causing loss of 10 to 20% of agricultural production world wide. Ground water will be vital to alleviate some of the worst drought situations. flooding and contaiminated water supplies, more intense weather events are likely to increase to risk of infectious disease epidemics and erosion of low-lying and costal land. Climate Chang will affect the quality of drinking Water and impact of fresh water availlablity and impact on public health it’s better to use UV Water purifiers. This paper will explore what climate change. Water is prime natural resources fulfilling our needs in a precisious assets.we must acts to preserve and utilize every drop of water. water resources can be assessed on the basis of surface and subsurface water bodies. Climate change imapact on ground Water the impact of climate change on ground water has been studied much less than the impact on surface waters. Ground water reacts to climate change mainly due to change in ground water recharge, but also change in river level in response to increase in mean Temperature, precipitation, variability and sea level as mean precipitations. Changing land use pattern due to increasing, urbanization, industrialization and agriculture activities are serious issues that causing increase ground water with drawal resulting in depletion of ground water resources and mining of ground water resources, along with deterioration of water quality. Rainfall is highly irregular and erratic and declining year to year due to change climatic conditions as result of serious global warming .Impacts of sea level rise on salinity intrusion global climate change has resulted in gradual sea level rise. sea level rise can cause saline water to migrate up stream in estuaries and rivers, thereby threating fresh water habitat and drinking- water supplies. Hydrology all the costal margin; fresh ground water flowing in land areas meets with saline ground water from the ocean. the fresh ground water flows from in land areas towards the coast where elevation and groundwater level are lower because salt water has higher content of dissolved salt and minerals. it denser the fresh water, causing it to have hydraulic head than freshwater. hydraulic head refers to the liquid pressure exerted by water column. the higher pressure density of salt water cause it to move into costal aquifiers in a wedge shape under the freshwater. the salt water and fresh water meets in a transition zone where mixing occurs through dispersion and diffusion.

Modelling of Coastal Vulnerability Index Along the East Coast of Peninsular Malaysia due to Sea Level Rise Impact

Sea level rise is a very serious phenomena around the world and caused by expansion of sea water due to the high temperature and the melting of ice at the poles. In Malaysia, areas located on the East Coast of Peninsular Malaysia are more vulnerable to the impact of rising sea water because they are facing the South China Sea where the waves are stronger, especially during the monsoon season in November to March. The study site is along the East Coast of Peninsular Malaysia, over 675km and covered fifteen districts located along the coast. This study focuses on developing vulnerability indices on physical, socioeconomic and correlation between both parameters. The analysis of physical vulnerability index (PVI) consist seven variables namely geomorphology, shoreline change rate, coastal slope, wave height, tidal range, sea level rise change and rock type. While for socioeconomic index (SeVI) focuses on three parameters such as quality of life, economic value and infrastructures. After obtaining the index for each parameter, coastal vulnerability index (CVI) is then calculated to determine the overall vulnerability for the coastal area. For CVI, the highest index along coastal area is Kuantan and the lowest index is Tumpat.

Experimental and Numerical Study to Investigate the Impact of Changing the Boundary Water Levels on Saltwater Intrusion in Coastal Aquifers

Experimental and numerical models can be used to investigate saltwater intrusion (SWI) in coastal aquifers. Sea level rise (SLR) and decline of freshwater heads due to climate change are the two key variables that may affect saltwater intrusion. This study aims to give a better understanding of the impact of increasing seawater levels and decreasing freshwater heads due to climate change and increasing abstraction rates due to overpopulation using experimental and numerical models on SWI. The experimental model was conducted using a flow tank and the SEAWAT code was used for the numerical simulation. Different scenarios were examined to assess the effect of seawater rise and landside groundwater level decline. The experimental and numerical studies were conducted on three scenarios: increasing seawater head by 25%, 50% and 75% from the difference between seawater and freshwater heads, decreasing freshwater head by 75%, 50% and 25% from the difference between seawater and freshwater heads, and a combination of these two scenarios. Good agreement was attained between experimental and numerical results. The results showed that increasing the seawater level and decreasing freshwater head increased saltwater intrusion, but the combination of these two scenarios had a severe effect on saltwater intrusion. The numerical model was then applied to a real case study, the Biscayne aquifer, Florida, USA. The results indicated that the Biscayne aquifer is highly vulnerable to SWI under the possible consequences of climate change. A 25 cm seawater rise and 28% reduction in the freshwater flux would cause a loss of 0.833 million m3 of freshwater storage per each kilometer width of the Biscayne aquifer. This study provides a better understanding and a quantitative assessment for the impacts of changing water levels’ boundaries on intrusion of seawater in coastal aquifers.

Genetically engineered heat-resistant coral: An initial analysis of public opinion.

Rising seawater temperatures are contributing to coral degradation in the Great Barrier Reef. Synthetic biology technologies offer the potential to enhance coral resilience to higher water temperatures. To explore what the public think of genetically engineered coral as a future solution, qualitative responses to an open-ended question in a survey of 1,148 of the Australian public were analysed. More respondents supported the technology (59%) than did not (11%). However, a considerable proportion indicated moderate support (29%). Participants commented about the (moral) right to interfere with nature and uncertainty regarding the consequences of implementing the technology. Participants also mentioned the need to take responsibility and act to save the reef, as well as the benefits likely to result from implementing the technology. Other themes included a desire for further testing and proof, more information, and tight regulation and controls when introducing the technology.

Preface

2nd International Conference on Cultural Communication & Space (ICCCS) CLIMATE CHANGE AND THE BUILT ENVIRONMENT Level 1, GDLN Building, Udayana University Denpasar CampusJl. P.B. Sudirman, Denpasar - Bali (80232), Indonesia5 August 2021https://icccs.unud.ac.id Gusti Ayu Made Suartika In 1896 the Swedish scientist and Noble Prize winner Svante Arrhenius showed that a doubling of atmospheric carbon dioxide would result on earth in increased surface temperature of 5-6 degrees Celsius. His warning has largely gone unheeded for the last 124 years, and we are already in an era of disaster management now guaranteed to get significantly worse. The response of nature is ubiquitous and terrifying-prolonged drought, bushfires, extreme flooding, unbearable heat waves, freezing storms, rising sea water levels, melting polar icecaps and glaciers, coastal abrasion, and other phenomena. Some believe these conditions are natural - the adopted manner by which the earth chooses to rejuvenate itself and therefore to deny we have any responsibility for its effects. Climate change sceptics promote ‘fake news’ largely to perpetuate business interests for a few more years, in a lemming like rush towards disaster. Or as O’Connor’s second law states, ‘capitalism always destroys the source of its own success.’Nature’s responses to centuries of abuse do not however address the human cost of global warming – everything from health issues, increasing costs of social services, the loss of livelihood and property, and the potential adaptation of our entire built environment in the interests of survival. The 2nd International Conference on Cultural Communication and Space (ICCCS) promotes the viewpoint that concerted action is needed across a wide range of offensives – providing alternative energy sources; remodelling the built environment; reducing both personal and industrial consumption of nature, radically changing political systems, an immediate triple bottom line approach to all business, and a sceptical view of technology as having any capacity to ameliorate the above problems. Even then a sustainable planet might not result.While many academic events have discussed these matters across the whole spectrum of problems, we focus here on the built environment in relation to climate change phenomena and its required responses to culture and space. Given the above considerations, this second ICCCS focuses on the following topics of conversation that address the significant policies and practices of climate change:List of CONFERENCE INFORMATION are available in this pdf.

ANTISIPASI TERJADINYA PEMANASAN GLOBAL DENGAN DETEKSI DINI SUHU PERMUKAAN AIR MENGGUNAKAN DATA SATELIT


 Remote sensing data has capability to detect Water Surface Temperatures in spatial or temporal analysis. Sea surface water temperature (SST) is one of the important indicators of dynamic global climate and dynamic regional climate. The increasing of SST will be effect to global warming and climate change and resulting in disaster such as hurricane, extreme heavy rain, landslide, tornado, melting ice in polar that resulting sea water rises. Indonesia as an Archipelago that consist of ten thousand islands, sea water rise scan cause a small island to sink. This research is aim to early detect SST with Remote Sensing to anticipate Global Warming. The method is literature study from related science journal as a result from researchers. Result of scientist’s researchers in Indonesia show that there has been increase of water surface temperature that has been varied in period over 32 years.It is need an effort to anticipate that there is no disaster.
 
 Keywords: Satellite Data;Global Warming;Remote Sensing;Surface Water Temperature