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<ul><li><div style='text-align:left;'><span style='text-align:center;'><b>Coastal Flood (UNOSAT 2022) </b>- Coastal Flood have generated maps from DEMs with height
above sea level and considered area that have height above sea level as</span></div><span><div style='text-align:left;'><span style='text-align:center;'>0 - 2 m. (High risk), 2 - 4 m. (Risk), 4 - 6 m. (Moderate), 6-8 m (Low
risk), and 8-10 m (Very low risk)</span></div></span></li><li><div style='text-align:left;'><span style='text-align:center;'><b>Flood susceptibility (UNOSAT 2022)</b> - maps using simplistic relative DEMs (Height Above Nearest Drainage Method).</span></div><span><span style='text-align:center;'><div style='text-align:left;'>considered area that have height above nearest river as <br />0-2 m (High Risk), 2-4 m (Risk), 4-6 m (Moderate), 6-8 m (Low Risk), and 8-10 m (Very Low Risk)</div></span></span></li><li><div><b>Earthquake (PacGeo 2017) </b>- An earthquake hazard map provides, at any location, the value of a ground motion intensity measure (for example, horizontal peak ground acceleration, PGA) that is expected to be exceeded at least once in 500 year mean return period. </div></li><li><div><b>Tropical cyclone wind (PacGeo 2017)</b> - A tropical cyclone wind hazard map provides, at any location, the value of a wind intensity measure (for example, maximum 1 minute sustained wind speed for tropical cyclones) that is expected to be exceeded at least once in 100 year time period. <br /></div></li><li><div><b>Erosion (JRC 2021)</b> - The Occurrence Change Intensity map provides information on where surface water occurrence
increased, decreased or remained the same between 1984-1999 and 2000-2020. The occurrence difference
between epochs was computed for each pair and differences between all homologous pairs of months
were then averaged to create the surface water occurrence change intensity map. Areas where there
are no pairs of homologue months could not be mapped. The averaging of the monthly processing
mitigates variations in data distribution over time (that is, both seasonal variation in the distribution of
valid observations, temporal depth and frequency of observations through the archive) and provides a
consistent estimation of the water occurrence change.</div></li><li><div><b>Tsunami Run up Return Period 475 years (GAR 2015)</b> - The results of tsunami hazard in terms of run-up height for a return period of 475 years after the calculations made by the Norwegian Geotechnical Institute and Geoscience Australia in the framework of GAR13. For more details on the tsunami hazard model see NGI and GA (2014).</div></li><li><div><b>Storm Surge (SRTM 2020)</b> - Calculated by SRTM elevation which area less than 6.5 meter</div></li></ul> |