The global mean sea level is rising.
While the global mean sea level rose by 1.7 mm/year in the 20th century, satellite records show that there was a marked acceleration from 1993, with the sea level rising at 3 mm/year.
The graph below shows the rising trend in global mean sea levels and projections for the future.
Time series of global mean sea-level in the past and future. Source: Intergovernmental Panel on Climate Change (IPCC)
In its 2019 report, the IPCC estimates that by 2100, the global mean sea level may rise by 0.61-1.10 meters (relative to 1986-2005) if greenhouse gas emissions continue to increase.
Key factors driving sea-level rise include melting glaciers and ice sheets and thermal expansion of ocean water because of rising temperatures.
So, why is sea-level rise a problem?
For low-lying coastal zones and small islands, sea-level rise (SLR) could cause frequent flooding, permanent submergence, salt-water intrusion and increased subsidence. SLR also increases the impact of extreme weather events like storm surges, which will push further inland than they did before.
In urban areas, rising water levels put critical infrastructures such as roads, bridges, tunnels, railways, utilities and buildings at risk. With transportation, commerce, clean water and electricity all relying on these critical infrastructures, SLR will have economic consequences too.
A 2021 study estimates that permanent flooding could lead to a 0.19% drop in real GDP (assuming a 4.5 Representative Concentration Pathway (RCP)) by the year 2200.
Given that SLR is not uniform but varies regionally and locally, adaptation measures take different forms depending on the circumstance, as illustrated in the image below.
Types of responses to SLR (Source)
Choosing how to respond, therefore, starts with using decision support systems to assess future exposure and vulnerability to SLR.
SLR risk assessment requires elevation data which is collected using different sensors and methods. Examples are Synthetic Aperture Radar (SAR), tri-stereo imagery, or LiDAR. Digital Surface Models (DSMs) and Digital Terrain Models (DTMs) are the most common ways of representing the collected elevations.
Why are DSMs and DTMs important and how are they used to assess SLR risks for critical infrastructure? Let's find out.
A Digital Surface Model (DSM) captures the elevation of natural and artificial features on the Earth's surface. It is used for the detection of buildings, trees, telecommunication towers, highways, and other ground features. DSMs allow the extraction of 3D data on critical infrastructure.
NEXTMap One DSM at 1-meter spatial resolution showing the elevation of natural features, vegetation and the built environment (Source: UP42)
A Digital Terrain Model (DTM) represents elevations of the bare earth—free from natural and artificial features such as vegetation and buildings. DTMs are crucial for SLR modelling because the shape of the Earth’s surface affects how water flows over it.
NEXTMap One DTM at 1-meter spatial resolution bare earth surface where features such as buildings, vegetation and other infrastructure have been removed (Source: UP42)
Normalised DSM (nDSM) is a derivative product of DSM and DTM. It is obtained by subtracting the DTM from the DSM. Note that the DTM and DSM used should have a common horizontal and vertical datum.
The nDSM is important because it allows direct measurement of heights.
Contreras, Jhonatan & Sickert, Sven & Denzler, Joachim. (2020). Region-Based Edge Convolutions With Geometric Attributes for the Semantic Segmentation of Large-Scale 3-D Point Clouds. IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing. PP. 1-1. 10.1109/JSTARS.2020.2998037. (CC BY 4.0)
Find out everything you need to know about elevation models here.
Here are 4 broad steps highlighting how DSMs and DTMs are used to assess SLR risks.
The sea level varies geographically, i.e., depending on where you are, the sea level is different.
This variation gives rise to global mean sea level and regional (also known as local) sea level. What's the difference?
|Global Mean Sea Level||Regional/ Local Sea Level|
|What is it?||The average height of water in the world's oceans.||Height of ocean water with respect to a specific point on the adjacent coastal land.|
|What causes rising sea levels?||Global change in the volume of ocean water due to: 1) Melting glaciers and ice sheets, 2) Thermal expansion due to rising temperatures||Changes in the global mean sea level plus regional/ local factors such as: 1) Regional ocean circulation patterns, 2) Coastal land subsidence, 3) Non-uniform changes in temperature and salinity|
Note: Because of the regional/ local factors highlighted above, some areas may experience a higher SLR rate than that observed globally---hence regional relative SLR rates.
According to the 2019 IPCC Special Report on the Ocean, regional SLR differs by about 30% from the global average.
Map showing relative sea-level trends. (Source: NOAA)
Regional/ local water levels should be applied in SLR risk assessment. With this in mind, regional water levels can be determined by either:
Modelling the ocean surface based on local/ regional measurements at tide stations over a long time. Modelled sea level surfaces show the sea-level variations in the area of interest.
Interpolating the water surface using values from nearby tide gauges---used where there are no tide gauges within the area of interest.
Using a single value to represent the water level throughout the area of interest (known as a "bathtub" model). Used for small areas where there's only one tide gauge. High watermarks can also be adopted as a single value.
Since areas below high tide lines already experience submergence during high tides, the high water tide mark is often used as the reference water level. This ensures that SLR impacts are only mapped for areas where flooding is the exception rather than the norm.
Water surface elevations are usually based on tidal datums, e.g. mean high water. As such, they must be converted to the vertical datum used by the DTM and DSM, e.g., ellipsoidal heights.
For the U.S., VDatum is a tool that can convert between tidal datums, orthometric heights and ellipsoidal heights.
SLR risks can be modelled for a range of SLR values to evaluate "what if" scenarios. These may be based on future SLR projections at a specific time.
For example, if the future SLR projection is 1.5mm/year, you may choose to evaluate SLR risks yearly over 10 years, where:
Future Sea Water Level = Existing Water Level (obtained in Step 1) + SLR Projection
For the reliability of the resulting flood model, the SLR value used must be more than the vertical error of the DTM. According to the National Oceanic and Atmospheric Administration (NOAA), the general guideline is that the modelled SLR value should be at least twice the vertical accuracy of the elevation data.
This is to say that to model SLR risks over shorter periods, you need an accurate DEM. Sources include:
High-resolution aerial imagery like Hexagon Geospatial's aerial imagery which covers the United States, Europe and parts of Canada
Tri-stereo high-resolution satellite imagery
Synthetic Aperture Radar (SAR) data like that captured by TerraSAR-X satellite
Subtracting the DTM from the Future Sea Water Level (obtained in step 3 above) results in a map showing:
Areas at risk of flooding due to future SLR
Flood depth represented as positive values in the raster
Note: For a more accurate risk assessment, it is important to ensure that the water flows across the surface of the DTM as it would in the real world. This is known as hydrologic connectivity. Hydrologic connectivity ensures that low-lying areas behind an obstacle are flooded if there is a channel connecting them to the ocean. Some examples of means to improve hydrologic connectivity include cutting road fills at drainage structures or stream burning on the DTM.
To identify the critical infrastructures affected and to what level (depth), the flood map obtained above is overlaid on the nDSM. Infrastructure that intersects the flood map is affected infrastructure and those that do not are non-affected infrastructure.
Find out how you can use OpenStreetMap data and UP42 to map the impact of flooding.
For coastal areas---which are generally flat---the accuracy of the DTM used is crucial because small sea-level changes can have a huge impact on the extent of critical infrastructures affected.
The quality of input elevation data determines the minimum increments in SLR and minimum projected timelines. For example, while several elevation models exist for large-area assessment of SLR risks, a 2018 study showed that the existing global DEMS are inadequate for mapping fine SLR increments of less than 1 meter or future forecasting of fewer than 100 years.
The image below ranks the suitability of global elevation datasets for SLR modelling.
Ranking of elevation data sources for SLR modelling. The 1-m sea-level rise is marked, which shows that only the high-accuracy DEM sources are suitable for modelling sub-meter increments at high confidence levels. (Source: Gesch DB (2018) Best Practices for Elevation-Based Assessments of Sea-Level Rise and Coastal Flooding Exposure. Front. Earth Sci. 6:230. doi: 10.3389/feart.2018.00230) (CC BY 4.0)
The table below highlights some sources of global elevation data and their characteristics.
|Elevation Data Source||Type||Details|
|Shuttle Radar Topography Mission (SRTM)||DSM||30-meter spatial resolution; ±16m absolute vertical accuracy|
|WorldDEM||DSM||12-meter spatial resolution; 2.5 m absolute vertical accuracy|
|ASTER Global DEM||DSM||Global resolution of 90 meters and 30 meters in the United States; Vertical accuracy of 20 meters at a 95% confidence|
|NEXTMap||DSM & DTM||1 m spatial resolution with a vertical accuracy up to 1m at a 90% confidence interval; 5 m spatial resolution with a vertical accuracy of up to 1.6 m at a 90% confidence interval; 10 m spatial resolution with a vertical accuracy of up to 8.4 m at a 90% confidence interval|
|JAXA Global ALOS World 3D||DSM||5-meter resolution; 7 m at a 90% confidence interval|
Sea Level Rise (SLR) is not uniform globally but varies by region.
One reason for this is vertical land movements along coastal areas occasioned by:
Land subsidence or sinking, causing rapid sea-level rise relative to the coastline. Groundwater extraction and mining of oils and minerals can cause the land to sink.
Land uplift whose effect is reduced sea level rise relative to the coastline. Uplift may be a result of tectonic plate movements or soil deposits.
For this reason, it is important to use an up to date DTM that captures changes in topography when assessing SLR risks. This is especially important for sinking coastal cities such as New Orleans, Bangkok, and Ho ChiMinh City.
Subsidence rates for long-term ground displacement can be obtained by using Interferometric Synthetic Aperture Radar (InSAR) methods such as Persistent Scatterer Interferometry (PSI) techniques.
Vertical errors found in global DEMs may lead to inaccurate SLR risk assessment, especially in densely vegetated and built-up areas. This is because global DEMs are DSMs that contain surface features like trees and buildings. Consequently, they tend to overestimate elevations i.e. positive vertical bias.
Nonetheless, freely available global DEMs makes them a cost-effective option for areas without LiDAR-based DEMs.
Some global DEMs may be more suited for modelling SLR risks in natural environments. And yet others may work better for urban areas. So, it is crucial to select a global DEM that best models SLR risks for the area of interest.
Various studies have assessed the suitability of different global DEMs for coastal flooding. We highlight a few of their findings below.
An accuracy assessment of ASTER, SRTM, ALOS, and TanDEM-X DEMs for the island of Hispaniola found that TanDEM-X DTMs provide an effective approximation of LiDAR DTMs for coastal flood mapping in areas without LiDAR data.
An analysis of the implications of using Global DEMs for flood risk analysis in cities found that global DEMs result in an inaccurate assessment of the extent and impact of flooding in cities---as compared to LiDAR data. The authors recommend using multiple global DEMs alongside each other to get a better picture of SLR impacts.
Evaluation of the performance of freely available DEM products in different parts of the world with different topography and land cover concluded that the accuracy of the global DEMs depended greatly on the unique characteristics of each region, as presented in the box plots below.
Box plots of errors by land cover class for all global digital elevation models for the four study areas. SRTM and NASADEM data were not available for the Norwegian study area because of its high latitude. Land cover classes: 1, Closed forest; 2, Open forest; 3, Shrubs; 4, Herbaceous vegetation; 5, Cultivated area; 6, Urban / built-up area; 7, Bare land / sparse vegetation; 8, Wetland; 9, Snow and ice; 10, Water. Only existing land cover classes are plotted for each study area. (Source: Uuemaa, E.; Ahi, S.; Montibeller, B.; Muru, M.; Kmoch, A. Vertical Accuracy of Freely Available Global Digital Elevation Models (ASTER, AW3D30, MERIT, TanDEM-X, SRTM, and NASADEM). Remote Sens. 2020, 12, 3482.) (CC BY 4.0)
Sea levels are rising. Mitigating SLR risks for critical coastal infrastructure calls for monitoring and modelling of SLR impacts and taking locally appropriate adaptation measures.
Geospatial data and analytics provide the means to identify, monitor and forecast SLR risks, informing policies on disaster preparedness and decision making.
At the same time, investment in climate tech across various industries is growing with PwC reporting that climate tech now accounts for 14 cents of every venture capital dollar. At the centre of climate tech business models is the need for frequent, high-quality earth observation data and analysis capabilities.
With continued advances in machine learning and cloud computing capabilities, geospatial technologies enable the analysis of huge volumes of past, present, and future satellite data to deliver insights for climate change mitigation and adaptation.