Climate Change and Coastal Line Shifts: Advances in Remote
Sensing Monitoring
Yundi Yang
Sino-Canada School, Jiangsu, 215211, People’s Republic of China
Keywords: Climate Change, Coastal Line Shift, Remote Sensing Monitoring.
Abstract: Climate change significantly impacts coastal environments, prompting the need for advanced monitoring
techniques. This paper examines the critical role of remote sensing technology in monitoring the shifts
in coastal lines due to climate change. It provides a comprehensive review of the application of satellite
imagery, LiDAR, and other sensors in capturing multi-temporal changes in coastal environments. The
study underscores the importance of these technologies in assessing coastal erosion, sedimentation, and
sea-level rise, offering detailed insights that are vital for coastal management and climate change
adaptation strategies. The paper also discusses the challenges in data acquisition and processing,
highlighting the need for advanced data pre-processing techniques. Furthermore, it explores the potential
of integrating big data, cloud computing, and AI to enhance real-time monitoring and predictive
capabilities. The future outlook highlights the integration of multi-source remote sensing data, UAV
technology, IoT and edge computing, and deep learning for more accurate and efficient monitoring. The
paper concludes that the continuous advancement in remote sensing, coupled with emerging
technologies, will significantly contribute to the sustainable development of coastal zones.
1 INTRODUCTION
The coastline is the boundary between the ocean and
the mainland, and it is not only an important part of
topographic maps and nautical charts but also one of
the 27 surface elements recognized by the
International Geographical Data Committee (Wu &
Hou, 2016). Shaped by a combination of terrestrial,
marine, atmospheric, and human activities, the
coastline exhibits unique geographical features and
dynamic characteristics, with its position, direction,
and form constantly changing. The coastline holds
substantial ecological functions and resource value.
With advances in transportation, rapid population
growth, accelerated economic development, and
increasing geographical importance, the coastline has
become one of the most frequently and intensely
impacted areas by human activities. However, rapid
economic development and limited land resources
have led to significant changes in the natural
ecological environment of coastal areas. The
construction of various coastal projects and the rapid
development of regional economies have reduced the
natural attributes of the coastline, and the original
production capacity and ecological functions have
changed significantly (Wu & Hou, 2015). The change
of the coastline is a key research topic in the field of
environmental geosciences. In recent years, with the
intensification of global climate change, the rise in
atmospheric temperature has significantly affected
the morphology and evolution process of the
coastline, as well as having a profound impact on sea
level, ecosystems, and human activities.
To better comprehend these impacts, researchers
have widely applied remote sensing technology,
especially satellite imagery, to monitor and analyze
changes in the coastline. Remote sensing imagery
technology has significant advantages and potential
in this field. By using aerial or satellite sensors to
obtain multi-band (such as visible light, infrared,
microwave) data and converting it into digital images,
it enables people to obtain and analyze large-scale,
multi-temporal surface information (Liang et al.,
2018). With the continuous advancement of remote
sensing technology, high spatial resolution and high
spectral resolution satellite images have emerged one
after another, with rapid scanning capabilities. These
technologies are now widely used in environmental
monitoring and management, allowing us to identify
and extract various components of the coastal
228
Yang, Y.
Climate Change and Coastal Line Shifts: Advances in Remote Sensing Monitoring.
DOI: 10.5220/0013042800004601
Paper published under CC license (CC BY-NC-ND 4.0)
In Proceedings of the 1st International Conference on Innovations in Applied Mathematics, Physics and Astronomy (IAMPA 2024), pages 228-234
ISBN: 978-989-758-722-1
Proceedings Copyright © 2024 by SCITEPRESS Science and Technology Publications, Lda.
environment and their related information more
efficiently and conveniently.
This study summarizes the relevant information
on the application of remote sensing imagery in the
changes of the coastline under the influence of
atmospheric temperature, not only showing the
research results in this field, filling the gaps in
research, but also providing scientific support and
decision-making basis for dealing with the challenges
brought by climate change. Finally, it anticipates the
future developmental trajectories in this field.
2 APPLICATION OF REMOTE
SENSING TECHNOLOGY IN
COASTAL LINE MONITORING
The utilization of remote sensing technology in
coastal boundary detection is diverse, offering
extensive, efficient, and cost-effective methods for
monitoring coastlines. It has significantly contributed
to global research on coastal zones, offering technical
support for diverse areas including pollution in
coastal ecological environments, environmental
disasters, and the restoration and protection of coastal
habitats. Remote sensing can be divided into the
following categories according to its data sources and
acquisition methods:
Figure 1: Mind maps for remote sensing technology applications (Picture credit: Original).
Satellite remote sensing is a technology that uses
artificial satellites as platforms to obtain information
about the Earth's surface through sensors. It has the
characteristics of wide coverage, strong continuous
observation capability, and high temporal resolution.
For example, the application of satellite data such as
Landsat, Sentinel, MODIS, etc.
Aerial remote sensing is a technology that uses
aircraft, helicopters, airships, unmanned aerial
vehicles (UAVs), and other aircraft as platforms to
obtain information about the Earth's surface with
sensors.
Ground remote sensing is a remote sensing
activity carried out on the Earth's surface, mainly
referring to the use of LiDar, ground
photogrammetry, and other technologies for
surveying and monitoring. Currently, LiDAR
technology is widely used in atmospheric research,
sea level measurement, and glacier research, with the
characteristics of fast speed, strong anti-interference
capability, and high precision.
Despite the significant advantages of remote
sensing technology in coastal boundary detection, it
also faces numerous challenges, such as the adverse
effects of cloudy and rainy weather on optical image
quality, and inadequate monitoring of coastal soil
quality and vegetation biochemical parameters (Li et
al., 2016). Therefore, the data sources obtained
Climate Change and Coastal Line Shifts: Advances in Remote Sensing Monitoring
229
through different remote sensing methods must be
professionally pre-processed and appropriate analysis
methods must be adopted to accurately reflect the
actual topographical conditions and changes of the
remote sensing area.
Remote sensing image pre-processing technology
is a key step to ensure the usability and accuracy of
remote sensing data. Researchers usually adopt
geometric correction, image registration, cloud
removal, atmospheric correction, and other means.
Research progress has shown that there are
various methods to automatically extract coastlines
from remote sensing images, including threshold
segmentation methods, edge detection operator
methods, active contour model methods, polarization
methods, etc. Among them, the edge detection
operator method has a better extraction effect on the
coastline, the method is more mature, and it is easy to
implement (Wu & Liu, 2019).
3 RESEARCH PROGRESS ON
COASTAL LINE CHANGE
REMOTE SENSING
MONITORING
3.1 Monitoring of Coastal Erosion and
Sedimentation
Research advancements in coastal change and remote
sensing monitoring predominantly center on utilizing
remote sensing to monitor coastal erosion and
sedimentation, and to analyze spatiotemporal
dynamic changes in coastline features. Through
literature search, we can find that the main research
areas include:
Research on the dynamic changes of erosion and
sedimentation in the Yellow River Delta: Combining
remote sensing and GIS technology, the land erosion
and sedimentation in the Yellow River Delta region
were studied, and it was found that the land area in
the Yellow River Delta region changes year by year
under the dual action of sedimentation and marine
erosion of the Yellow River (Dong et al.).
Spatiotemporal evolution analysis of the coastline
in Greater Bay Area: Using remote sensing imagery
to obtain coastline data from 1975 to 2018, the
development and utilization of the coastline and the
spatial position changes were analyzed based on the
GIS platform (Yang et al., 2021).
Remote sensing monitoring of the status of coastal
erosion in Jiangsu Province: Using satellite remote
sensing interpretation, tidal numerical simulation,
and GIS spatial topological analysis, the current
status of coastal erosion in Jiangsu Province was
monitored (Cui et al.).
These studies show that remote sensing
technology has become an important tool for coastal
line change research, providing spatiotemporal
dynamic information on coastal erosion and
sedimentation, providing a scientific basis for coastal
zone management and protection.
3.2 The Impact of Sea Level Rise and
Climate Change
Sea level rise (SLR) is one of the most urgent
challenges of climate change, which has aroused
widespread research interest in recent years. It relates
to factors such as global warming, melting of polar
glaciers, and thermal expansion of the upper ocean
water. The rise in sea level caused by climate change
has a significant impact on coastline, and the climate-
driven factors mainly include two parts: first, factors
caused by changes in the atmosphere and ocean
(Sarrau et al., 2024), the rate of sea level rise is
affected by the intensity, height, and frequency of
waves in coastal and tidal areas (Chini ey al., 2010;
Aagaard &
Sørensen, 2012). In addition, linear sea
level rise scenarios and extreme events also affect
wave action in coastal areas. Another climate-driven
factor is the melting of land glaciers, which leads to
the influx of freshwater into the ocean. This not only
changes the density structure of the ocean but also
affects wave action. These impacts can be studied and
analyzed through remote sensing monitoring
technology (Li et al., 2020).
Specific monitoring methods divides into the
following categories:
Satellite radar altimeters
Satellite radar altimeters are widely used remote
sensing technologies for measuring sea level height.
This technology calculates changes in sea level height
by sending radar signals from satellites to the Earth's
surface and receiving the return signals. For example,
scientists have been able to monitor long-term trends
in global sea level changes using radar altimeter data
from a series of satellites such as TOPEX/Poseidon,
Jason-1, Jason-2, and Jason-3 (Allenbach et al.,
2015).
Satellite gravity measurement
The GRACE (Gravity Recovery and Climate
Experiment) satellite mission monitors the mass loss
of glaciers and ice caps and their contribution to sea
level rise by measuring changes in the Earth's gravity
field. For instance, Velicogna (Velicogna, 2009)
employed GRACE satellite data to quantify
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Greenland and Antarctic ice sheet mass loss,
elucidating their influence on global sea level rise.
Optical and radar imaging
Remote sensing imaging technologies, such as
optical and radar images from Landsat and Sentinel
series satellites, are widely used to monitor changes
in coastal areas. These images can capture changes in
coastlines, the submersion of wetlands, and the
degradation of salt marshes. For example, Murray et
al. (Murray et al., 2019) used Landsat images to
analyze changes in the area of global coastal wetlands
over the past few decades and assessed the impact of
sea level rise on these ecosystems.
The response of coastlines to climate change
varies across different regions, mainly due to
differences in geographical location, topography,
environmental conditions, and human activities. The
application of remote sensing monitoring technology
provides important data support and analysis methods
for studying the response of coastlines to climate
change. Here are some current research statuses in
this field.
The coastal areas of Bangladesh are among the
most severely affected areas by sea level rise globally.
Researchers have used multi-source remote sensing
data, including radar altimeters, optical and radar
imaging techniques, to monitor changes in the
coastline, flood risks, and wetland degradation in the
region (Sarwar & Woodroffe, 2013). For example,
Sarwar and Woodroffe (2013) used Landsat image
data to analyze long-term trends in the changes of the
coastline in Bangladesh, revealing the impact of sea
level rise and human activities on coastal erosion.
Similarly, the East Coast of US has also significantly
affected, especially due to the combined effects
The coastal areas of Bangladesh are among the
most severely affected regions globally by the rise in
sea levels. Researchers have utilized multi-source
remote sensing data, including radar altimeters,
optical and radar imaging techniques, to monitor the
changes in coastlines, flood risks, and wetland
degradation in these areas (Sarwar & Woodroffe,
2013). For instance, Sarwar and Woodroffe (2013)
employed Landsat imagery to analyze the long-term
trends in the changes of Bangladesh's coastline,
revealing the impacts of sea-level rise and human
activities on coastal erosion. Similarly, the East Coast
of the United States has also significantly affected,
particularly due to the combined effects of sea-level
rise and frequent extreme weather events, such as
hurricanes. These case studies not only demonstrate
the application of remote sensing technology in
monitoring and analysing sea-level rise but also
provide essential scientific support for the
development of effective coastal management and
adaptation strategies.
In China, the Jiangdong New Area of Haikou and
its neighbouring regions have also deeply affected by
the rise in sea levels. Utilizing Landsat data,
researchers have conducted remote sensing
monitoring and change characteristic analysis of the
coastline in this area from 1987 to 2018. Their
findings indicate that over the past 31 years, the
coastline has shown a trend of "decrease - increase -
stability" in its evolution, with a net increase of 1.52
km in total length, and human factors have become
the main driving force behind the changes in the
coastline (Zhu & Zhang, 2023). Additionally, remote
sensing technology plays a crucial role in monitoring
the coastal zone's geographical environment,
including land use/cover, soil quality, vegetation,
coastlines, water color, water depth, and underwater
topography, as well as disaster monitoring (Li et al.,
2016).
3.3 Changes in the Coastline under
Human Activities
Human activities have multifaceted impacts on
coastlines, including direct effects on coastal
morphology and coastal ecosystem structures, as well
as indirect effects on the socio-economic framework
of coastal zones.
Urbanization, port construction, and changes in
land use are significant human factors affecting the
evolution of coastlines. Specifically, urbanization
leads to the replacement of natural coastlines with
buildings and infrastructures as urban spaces expand,
affecting not only the natural form of the coastline but
also the ecosystem services of the coastal zone (Shi et
al., 2022). Port construction is another significant
human-induced factor of coastline change. The
establishment or expansion of ports requires
extensive land reclamation, which directly alters the
original state of the coastline. Additionally, changes
in land use, such as agricultural development,
industrial growth, and tourism expansion, can impact
the coastline. Specifically, land reclamation activities
not only change the form of the coastline but may also
cause damage to coastal wetlands and ecosystems
(Wei wt al., 2019).
Remote sensing monitoring technology plays a
pivotal role in studying changes in coastlines and
their impacts, especially when analyzing the effects
of human activities on these changes. For example, in
China's Pearl River Delta, due to large-scale land
reclamation and industrial development, the coastline
has undergone rapid changes, and the ecosystem has
Climate Change and Coastal Line Shifts: Advances in Remote Sensing Monitoring
231
been significantly affected (Tang et al., 2010).
Similarly, the coast of Mandla in India has notably
influenced by human activities due to port
construction and sand mining (Jayappa & Narayana,
2009). In Florida, USA, research has found that
coastal erosion has intensified due to the expansion of
real estate development and tourism (Passeri et al.,
2018). Remote sensing technology enables
researchers to accurately monitor these changes and
assess their long-term impacts. For instance,
Luijendijk et al. (2018) analyzed global coastline
changes using a satellite dataset, revealing the
significant impact of human activities on coastline
changes worldwide (Luijendijk et al., 2018).
Menaschiro et al. (2018) also used remote sensing
data to study the driving factors behind global
coastline retreat, including human activities and
natural processes (Mentaschi et al., 2018).
In summary, through remote sensing monitoring,
scientists can more accurately understand the changes
in coastlines, assess the impact of climate change on
coastlines, and provide a scientific basis for the
management and protection of coastal zones.
4 FUTURE RESEARCH
OUTLOOK AND PROSPECTS
FOR REMOTE SENSING
MONITORING OF COASTAL
LINE CHANGES
Monitoring coastline changes using remote sensing
technology is a continually evolving field, with future
research directions deeply influenced by current new
technologies, the results of which can be widely
applied to the management and policy of coastline
protection.
4.1 Big Data and Cloud Computing in
Monitoring Coastal Changes
For new technologies, big data, cloud computing, and
artificial intelligence have broad application
prospects in monitoring coastal changes:
Big Data Technology
Capable of processing and analyzing massive
amounts of data collected from various sensors and
remote sensing equipment, including satellite images,
topographic data, and meteorological data, which are
crucial for understanding the dynamic changes of
coastlines.
Cloud Computing
Provides the necessary computational resources
and storage capacity to handle big data, with its
elasticity and scalability allowing resources to be
dynamically adjusted according to demand.
Artificial Intelligence and Machine Learning
Improve the accuracy and efficiency of automatic
coastline extraction, enabling real-time monitoring
and trend prediction on a larger scale, providing a
scientific basis for regulation and protection.
With ongoing advancements in remote sensing
technology and AI implementation, outcomes will
furnish precise data for coastline safeguarding and
management, anticipate trends and risks in coastline
alterations, and foster proactive and effective coastal
protection measures, bolstering responsiveness to
climate change.
4.2 Multi-Source Remote Sensing Data
Integration
By integrating remote sensing data from different
sources (such as optical remote sensing, radar remote
sensing, LiDAR, etc.), more comprehensive and
accurate information on coastline changes can be
obtained. This multi-source data integration method
can overcome the limitations of single data source
and improve the reliability and accuracy of results.
4.3 Application of UAV Technology
UAVs, with their high resolution, flexible mobility,
and low cost, can be used for high-frequency and
small-scale coastline monitoring, especially suitable
for areas that are difficult to cover by traditional
satellite remote sensing. The development of UAV
technology will further enhance the fine monitoring
capabilities of local coastline changes.
4.4 IoT and Edge Computing
Deploying IoT sensors near coastlines can collect
real-time environmental data (such as tides, waves,
wind speed, etc.), and combining edge computing
technology for preliminary data processing and
analysis locally can provide real-time feedback on
changes, improving the timeliness and accuracy of
monitoring.
4.5 Application of Deep Learning
Technology
Deep learning has significant advantages in image
and pattern recognition and can be used to
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automatically extract coastline features from remote
sensing images, classify and identify different types
of coastline changes, thereby improving monitoring
efficiency and accuracy. This includes establishing
real-time monitoring and early warning systems
based on remote sensing data, which can dynamically
monitor coastline changes, timely detect and warn
potential risks such as coastal erosion and storm
surges, providing real-time decision support for
managers.
4.6 Integration of Remote Sensing Data
with Socio-economic Data
By combining remote sensing monitoring data with
socio-economic data—such as land use, population
distribution, and economic activities—a
comprehensive analysis can be conducted. This
analysis can assess the impact of coastline changes on
socio-economic development and formulate more
scientifically sound policies for protection and
management. Furthermore, enhancing global and
regional-scale monitoring of coastline changes
through international collaboration and data sharing
can establish a worldwide network for monitoring
such changes, offering data backing and a decision-
making foundation for global coastline protection and
management.
These research directions will further enhance the
capabilities of remote sensing monitoring for
coastline changes, offering stronger technical support
for climate change adaptation and coastline
protection.
Figure 2: Mind map of Future Research Outlook and Prospects for Remote Sensing Monitoring of Coastal Line Changes
(Picture credit: Original).
5 CONCLUSION
In conclusion, remote sensing technology has become
an essential tool for monitoring the changes in
coastlines. It acquires multi-temporal and multi-
spectral data through satellites, aerial, and ground
sensors, providing spatiotemporal dynamic
information on coastal erosion, sedimentation, and
sea-level rise. Technological advancements have
improved monitoring efficiency with high-resolution
imaging and rapid scanning capabilities. Future
research will leverage big data, cloud computing, and
artificial intelligence to further enhance data
Climate Change and Coastal Line Shifts: Advances in Remote Sensing Monitoring
233
processing capabilities and the precision of automatic
extraction, achieving real-time monitoring and trend
forecasting. This will establish a scientific foundation
for coastline protection, policy formulation, and
climate change adaptation strategy development,
thereby fostering sustainable coastal zone
development.
REFERENCES
Wu, T., & Hou, X. (2016). A review of coastal line change
research. Acta Ecologica Sinica, 36(4), 1170-1182.
Wu, T., & Hou, X. (2015). A review of domestic and
international coastal line change research. Acta
Ecologica Sinica, 36(4), 13.
Liang, L., Liu, Q., Liu, G., Li, X., & Huang, C. (2018). A
review of coastal line extraction methods based on
remote sensing imagery. Journal of Geo-Information
Science, 20(12), 11.
Li, Q., Lu, Y., Hu, S., Hu, Z., Li, H., Liu, P., Shi, T., Wang,
C., Wang, J., & Wu, G. (2016). Review of remotely
sensed geo-environmental monitoring of coastal zones.
Journal of Remote Sensing, 20(5), 1216-1229.
https://doi.org/10.11834/jrs.20166168
Wu, Y., & Liu, Z. (2019). Research progress on methods of
automatic coastline extraction based on remote sensing
images. Journal of Remote Sensing, 23(4), 582-602.
https://doi.org/10.11834/jrs.20197410
Dong, F., Zhao, G., Tian, W., & Fan, R. (n.d.). [No
publication year]. [No article title provided]. [Journal
name not provided].
Yang, C., Gan, H., Wan, R., & Zhang, Y. (2021).
Spatiotemporal evolution and influencing factors of the
coastline in the Guangdong-Hong Kong-Macao Greater
Bay Area from 1975 to 2018. Chinese Geology, 48(3),
697-707. https://doi.org/10.12029/gc20210302
Cui, D., Lyu, L., Zhou, Y., Deng, H., Zhang, H., Zhang, D.,
& Shen, Y. (n.d.). [No publication year]. [No article
title provided]. [Journal name not provided].
Li, P., Pu, S., Li, Z., & Wang, H. (2020). Coastline change
monitoring of Jiaozhou Bay from multi-source SAR
and optical remote sensing images since 2000.
Geomatics and Information Science of Wuhan
University, 45(9), 1485-1492.
https://doi.org/10.13203/j.whugis20180483
Zhu, X., & Zhang, Y. (2023). The change analyses of
shoreline in Jiangdong New District and its adjacent
region, Haikou. South China Geology, 39(1), 127-137.
https://doi.org/10.3969/j.issn.2097-0013.2023.01.011
Li, Q., Lu, Y., Hu, S., Hu, Z., Li, H., Liu, P., Shi, T., Wang,
C., Wang, J., & Wu, G. (2016). A review of remote
sensing monitoring of coastal zone geo-environment.
Journal of Remote Sensing, 20(5), 1216-1229.
Shi, J., Li, W., Liu, Y., Zhou, W., Han, L., Tian, S., Wang,
Y., & Niu, X. (2022). Impacts of urbanization on
coastline and coastal zone in the Guangdong-Hong
Kong-Macao Greater Bay Area. Acta Ecologica Sinica,
42(1), 67-75.
Wei, F., Han, G., Han, M., Zhang, J., Li, Y., & Zhao, J.
(2019). Temporal-spatial dynamic evolution and
mechanism of shoreline and the sea reclamation in the
Bohai Rim during 1980-2017. Scientia Geographica
Sinica, 39(6), 997-1007.
https://doi.org/10.13249/j.cnki.sgs.2019.06.015
Sarrau, J., Alkaabi, K., & Bin Hdhaiba, S. O. (2024).
Exploring GIS techniques in sea level change studies:
A comprehensive review. Sustainability, 16(7), 2861,
192204. https://doi.org/10.3390/su16072861
Chini, N., Stansby, P., Leake, J., Wolf, J., Roberts-Jones, J.,
& Lowe, J. (2010). The impact of sea level rise and
climate change on inshore wave climate: A case study
for East Anglia (UK). Coastal Engineering, 57(11
12),973-984.
Aagaard, T., & Sørensen, P. (2012). Coastal profile
response to sea level rise: A process-based approach.
Earth Surf. Process. Landforms, 37, 354-362.
https://doi.org/10.1002/esp.2271
Allenbach, K., Garonna, I., Herold, C., Monioudi, I.,
Giuliani, G., Lehmann, A., & Velegrakis, A. F. (2015).
Black Sea beaches vulnerability to sea level rise.
Environmental Science & Policy, 46, 95-109.
https://doi.org/10.1016/j.envsci.2014.07.014
Velicogna, I. (2009). Increasing rates of ice mass loss from
the Greenland and Antarctic ice sheets revealed by
GRACE. Geophysical Research Letters, 36(19).
Murray, N. J., Phinn, S. R., DeWitt, M., Ferrari, R.,
Johnston, R., Lyons, M. B., et al. (2019). The global
distribution and trajectory of tidal flats. Nature,
565(7738), 222-225.
Sarwar, M. G. M., & Woodroffe, C. D. (2013). Rates of
shoreline change along the coast of Bangladesh. Journal
of Coastal Conservation, 17(3), 515-526.
Tang, X., Liu, S., Liu, J., et al. (2010). Effects of vegetation
restoration and slope positions on soil aggregation and
soil carbon accumulation on heavily eroded tropical
land of Southern China. Journal of Soils and Sediments,
10, 505
513. https://doi.org/10.1007/s11368-009-
0122-9
Jayappa, K. S., & Narayana, A. C. (2009). Influence of
coastal structures on the beaches of southern Karnataka,
India: A study using remote sensing data. Journal of
Coastal Research, 25(1), 264-273.
Passeri, D. L., Long, J. W., Plant, N. G., Bilskie, M. V., &
Hagen, S. C. (2018). The influence of bed friction
variability due to land cover on storm-driven barrier
island morphodynamics. Coastal Engineering, 132, 82-
94.
Luijendijk, A., Hagenaars, G., Ranasinghe, R., Baart, F.,
Donchyts, G., & Aarninkhof, S. (2018). The state of the
worlds beaches. Scientific Reports, 8(1), 6641.
Mentaschi, L., Vousdoukas, M. I., Pekel, J. F.,
Voukouvalas, E., & Feyen, L. (2018). Global long-term
observations of coastal erosion and accretion. Scientific
Reports, 8(1), 12876.
IAMPA 2024 - International Conference on Innovations in Applied Mathematics, Physics and Astronomy
234