Mr Wagner Luiz Langer Costa
Prediction of coastal flooding events within New Zealand. Important to have some capability to describe the event, and its impact on the environment. An area of particular concern is the estimation of bathymetry data for estuaries.
A number of parameters are taken into consideration when arriving at a calculation related to sea level including: mean sea level, astronomical tide, storm surge, wave run-up, fluvial discharge and vertical land motion. There are three main ways in which bathymetry can be calculated. These include, RTK - Real-time kinematics, Echo sounders and LiDAR, Remote Sensing. Of the three, Remote Sensing is the most economical, however it suffers from the lowest accuracy of the three approaches.
The Copernicus programme uses satellites for earth observation missions with an intended outcome being the delivery, free of charge, of data captured using these instruments.
Objectives - Generate satellite derived bathymetry measurements for all estuaries within New Zealand, especially those having little, or non-existent bathymetric data.
This research will be conducted within Tauranga Harbour, Bay of Plenty geographic area.
Need to process terabytes of raw data in order to arrive at a satisfactory conclusion. Processing must be concluded within a finite time window.
Extract data from Google Earth Engine. Estimate bathymetry and compare to results obtained using LiDAR.
Notebook: 'Estimating bathymetry in intertidal zone from sentinel ESA satellite images'
Google Colab provides an environment for hosting and executing of Jupyter notebooks. Colab frees the researcher's personal computer for other tasks with the computational workload executed on cloud based resources.
Tutorial Video 1 (shown below)
Tutorial Video 2