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Relation of extreme precipitation with temperature: How do open-access global gridded datasets work in a hydrometeorological study?

Analysts have long noted that extreme precipitation appears to intensify with temperature at a rate of around 7%/°C, which is governed by the Clausius-Clapeyron (CC) equation. This study aims to investigate the relationship between the spatio-temporal properties of hourly precipitation and daily dew point temperature. Specifically, the global gridded products of bias-corrected Climate Prediction Center morphing technique (CMORPH-CRT) and ERA5 reanalysis were applied for nine locations in the world. The results show that significant spatial heterogeneity in extreme precipitation scaling is present at the selected locations, which might be attributed to local conditions, such as regional climate and the proximity to humidity sources. Despite the potential limitations, this study provides insight into the application of high-resolution open-access global gridded products in analysing precipitation scaling.

Event

Local Perspectives Case Studies

Map

Click on any of the highlighted countries to retrieve further information.

Person

Space-based Solution

Addressed challenge(s)

Lacking historic knowledge on vegetation cover and surface water extent / river course

Collaborating actors (stakeholders, professionals, young professionals or Indigenous voices)
Suggested solution

Note: this description is a work in progress developed by the collaborating entities in a workshop. If you would like to contribute reach out to office@space4water.org, or your trusted Space4Water point of contact.

The solution approach begins with identifying the region's main rivers and understanding their hydrology using mapping and geoprocessing tools. After understanding the hydrography of the area and mapping the surface water extent river course through the building a hydrographic dataset, multiple image sources are used to map the historical land use and land cover surrounding the river.

1. Resources needed

Software

  • QGIS https://www.qgis.org/en/site 
  • TerraHidro 5 - Console applications https://www.dpi.inpe.br/terrahidro/doku.php
  • PostgreSQL https://www.postgresql.org
  • PostGIS Spatial Database System  https://postgis.net/
  • PgHydro extension for PostgreSQL/PostGIS http://pghydro.org/
  • PgHydro Plugin for QGIS https://plugins.qgis.org/plugins/PghydroTools/

Data

Forest And Buildings removed Copernicus DEM

Publications

see reference in the bibliography below.

2. Steps to the solution & status

Overivew

  1. Plot the Region of Interest (completed)
  2. Identify the region's main rivers and understand their hydrology (completed);
  3. Identify the region's potential flood areas using H.A.N.D.;
  4. Build a hydrography dataset (completed);
  5. Identify multiple image sources for land cover analysis (completed);
  6. Map the historical land use and land cover surrounding the river (in progress);

Step-by-step

1. Plot the Region of Interest (completed)

  1. Download and install QGIS to plot the KML files of the region of interest
Example KML plot of the strip of land of the Maori communtiy who submitted the challenge
Figure 1: Example KML plot of the strip of land of the Maori communtiy who submitted the challenge

 

2. Identify the region's main rivers and understand their hydrology (completed)

  1. Download the FABDEM data for the Region of Interest.
    FABDEM (Forest And Buildings removed Copernicus DEM) is a global elevation map that removes building and tree height biases from the Copernicus GLO 30 Digital Elevation Model (DEM) (https://data.bris.ac.uk/data/dataset/25wfy0f9ukoge2gs7a5mqpq2j7).
     
    A FEABDEM Digital Elevation Model of the Ngutunui region, New Zealand.
    Figure 2: A FEABDEM Digital Elevation Model of the Ngutunui region, New Zealand.

     
  2. Download and Install TerraHidro 5 - Console applications (https://www.dpi.inpe.br/terrahidro/doku.php) to extract the hydrograph products derived from the FABDEM to understand the hydrography setup of the area (Flow direction, flow accumulation and drainage lines and areas, H.A.N.D.).
     
    Flow direction in the Ngutunui region, New Zealand
    Figure 3: Flow direction in the Ngutunui region, New Zealand
    Flow accumultation in the Ngutunui region, New Zealand
    Figure 4: Flow accumultation in the Ngutunui region, New Zealand
     
    Sintetetic drainage lines and areas
    Figure 5: Sintetic draingage lines and areas Ngutunui region, New Zealand

     

3. Identify the region's potential flood areas using H.A.N.D.

Building on Nobre et. al (2011) in which the HAND terrain model that "normalizes topography according to the local relative heights found along the drainage network, and in this way, presents the topology of the relative soil gravitational potentials, or local draining potentials" is introduced by the authors.

Height Above the Neaerest Drainage (HAND)in the Ngutunui reiong,
Figure 6: Height Above the Neaerest Drainage (HAND) in the Ngutunui region showng the areas for potential flooding in darker blue. In the current map this is in the bottom right quarter of the image.

 

4. Build a hydrography dataset (completed)

  1. Download and instal PostgreSQL/PostGIS Spatial Database System (https://www.postgresql.org/) (https://postgis.net/), PgHydro extension for PostgreSQL/PostGIS (http://pghydro.org/) and PgHydro Plugin for QGIS;(https://plugins.qgis.org/plugins/PghydroTools/).
  2. Build the Hydrograph Dataset;(https://www.youtube.com/channel/UCgkCUQ-i72bBY41a1bhVWyw) using the Drainage Lines and Drainage Areas extracted from FABDEM;
  3. Information like drainage area, upstream area, drainage line length and distance to sea information are now available.
     
    Hydrography dataset of the Ngutunui region in New Zealand
    Figure 7: Hydrography dataset of the Ngutunui region in New Zealand

     

5. Identify multiple image sources for landing cover analysis (completed);

  1. To collect historic and high-resolution up-to-date imagery over the area, UNOOSA contacted the Land and Information New Zealand Data Service, which provided both historical aerial imagery and LIDAR data sources.
  2. Historic data for the relevant land patch can be accessed via the Retrolens New Zealand Service (https://retrolens.co.nz/Map/#/1784971.9859981549/5783474.532151884/1786387.2653498782/5784857.564632303/2193/12).
  3. Up-to-date aerial photos of the area can be accessed here at the New Zealand Data Service. Tile 503 and 603 are the ones of interest (https://data.linz.govt.nz/layer/112048-waikato-03m-rural-aerial-photos-index-tiles-2021-2023/history/).
  4. Relevant Landsat data are available from 1989. For the study area, Landsat 7 data is available from 2 July 1999, and Landsat 4 from 2 February 1989;
  5. Google Earth Engine Apps - Global Forest Change (https://google.earthengine.app/view/forest-change)

6. Map the historical land use and land cover surrounding the river (in progress);

Relevant publications
Related space-based solutions
Keywords (for the solution)
Climate Zone (addressed by the solution)
Habitat (addressed by the solution)
Region/Country (the solution was designed for, if any)
Relevant SDGs