Dry climates are represented within the climate group: Dry
They are characterized by the amount of annual precipitation less than a threshold value which approximates the potential evapotranspiration.
The threshold value (in mm) is calculated as follows:
Multiply the average annual temperature in °C by 20, then add
(a) 280 if 70% or more of the total precipitation is in the high-sun half of the year (April through September in the Northern Hemisphere, or October through March in the Southern), or
(b) 140 if 30%–70% of the total precipitation is received during the applicable period, or
(c) 0 if less than 30% of the total precipitation is so received.
According to the modified Köppen classification system used by modern climatologists, total precipitation in the warmest six months of the year is taken as reference instead of the total precipitation in the high-sun half of the year.[19]
If the annual precipitation is less than 50% of this threshold, the classification is Arid: desert climate. Arid climates can be classified as either hot or cold deserts.
Dr. Nivin Hasan discusses her pioneering work in space technology and water resource management, emphasising the role of remote sensing and geographic information systems (GIS) in addressing climate challenges in Jordan and the Middle East and North Africa (MENA) region. She highlights her research on drought assessment in the Amman-Zarqa Basin using satellite data and machine learning, underscoring the need for innovative solutions in arid zones. As a Technical Advisor at Royal Jordanian Geographic Centre (RJGC), she oversees projects integrating geospatial analysis for sustainable groundwater management and disaster resilience.
Her proudest achievements include leading Jordan’s first CANSAT project and receiving global recognition for empowering women in STEM. She identifies water scarcity, climate variability, and data gaps as critical challenges in arid regions and advocates for space-based monitoring systems to enhance mitigation strategies.
Dr. Hasan encourages young women to pursue space science, stressing mentorship and perseverance. She calls for interdisciplinary collaboration and funding to drive innovation in environmental monitoring. When asked about her favourite aggregate state of water, she humorously notes its irrelevance to her research but acknowledges the symbolic importance of liquid water for life in arid landscapes.
Margherita is an interdisciplinary Earth scientist and drone pilot with a background in geologic and environmental sciences. She has international experience working in fields such as Earth Observation (EO), remote sensing, drones & geospatial data analysis applied to the environmental and humanitarian sectors, sustainability and climate change. Margherita is passionate about natural and climate-related technologies that can be used to develop sustainable and long-lasting solutions. She is working for a more inclusive world (Women in Geospatial+), without any sort of geographical or social barriers.
Keywords: Science communication, Climate Change, STEM, inclusivity, sustainability, nature, hydrosphere, hydrology, water risks, Earth Observation (EO), satellite data, flood modeling, vulnerability, resilience, lifelong learning
Region/Country mentioned: Temperate climates, Arid climates, Luxembourg, Niger
Relevant SDG targets: 1, 4, 6, 9, 11, 13, 17
Dr. Nivin Hasan discusses her pioneering work in space technology and water resource management, emphasising the role of remote sensing and geographic information systems (GIS) in addressing climate challenges in Jordan and the Middle East and North Africa (MENA) region. She highlights her research on drought assessment in the Amman-Zarqa Basin using satellite data and machine learning, underscoring the need for innovative solutions in arid zones. As a Technical Advisor at Royal Jordanian Geographic Centre (RJGC), she oversees projects integrating geospatial analysis for sustainable groundwater management and disaster resilience.
Her proudest achievements include leading Jordan’s first CANSAT project and receiving global recognition for empowering women in STEM. She identifies water scarcity, climate variability, and data gaps as critical challenges in arid regions and advocates for space-based monitoring systems to enhance mitigation strategies.
Dr. Hasan encourages young women to pursue space science, stressing mentorship and perseverance. She calls for interdisciplinary collaboration and funding to drive innovation in environmental monitoring. When asked about her favourite aggregate state of water, she humorously notes its irrelevance to her research but acknowledges the symbolic importance of liquid water for life in arid landscapes.
Margherita is an interdisciplinary Earth scientist and drone pilot with a background in geologic and environmental sciences. She has international experience working in fields such as Earth Observation (EO), remote sensing, drones & geospatial data analysis applied to the environmental and humanitarian sectors, sustainability and climate change. Margherita is passionate about natural and climate-related technologies that can be used to develop sustainable and long-lasting solutions. She is working for a more inclusive world (Women in Geospatial+), without any sort of geographical or social barriers.
Keywords: Science communication, Climate Change, STEM, inclusivity, sustainability, nature, hydrosphere, hydrology, water risks, Earth Observation (EO), satellite data, flood modeling, vulnerability, resilience, lifelong learning
Region/Country mentioned: Temperate climates, Arid climates, Luxembourg, Niger
Relevant SDG targets: 1, 4, 6, 9, 11, 13, 17
The proposed solution leverages Earth Observation (EO) and climate data to develop a machine learning-based irrigation demand forecasting system tailored for smallholder farmers operating under the Warabandi system. In regions where rotational irrigation governs water distribution, farmers often lack accurate tools to forecast short-term irrigation needs, leading to overuse or underuse of water, both of which impact productivity and efficiency. This space-based solution addresses the challenge by integrating EO-derived variables such as Normalized Difference Vegetation Index (NDVI), Soil-Adjusted Vegetation Index (SAVI), Land Surface Temperature (LST), and net radiation to estimate actual crop water requirements. The model enables data-driven decision-making for farmers and water managers, promoting more efficient and timely irrigation practices within fixed rotation systems.
Donor: Water Resource Accountability in Pakistan (WRAP), supported by the Foreign, Commonwealth & Development Office (FCDO)
Government Departments Involved: On-Farm Water Management (OFWM), Agriculture Department and Irrigation Department, Punjab
Community and Sectoral Engagement: Farmers’ associations and local water user groups, experts in water demand management from academia and the private sector
Inclusive Participation: Integrating voices from underrepresented communities, including women and Indigenous stakeholders.
Requirements
Data
Landsat time series
PlanetScope time series
Climate data: ERA5 (Copernicus), Flux Tower System (for validation)
Crop calendar and landcover data integrated with ML models
Google Colab: Python-based model training and automation
Python, TensorFlow/PyTorch for ML model setup
Physical
Validation of land cover features, historical crop water use, and weather parameters through ground-based systems such as flux tower, along with crop information verified using crop calendars and spectral signatures collected from the field.
The information regarding soil moisture will be verified through Soil moisture sensors.
Outline steps for a solution
Data collection and sourcing (Completed)
Workflow development and EO dataset integration (In progress)
Data loader development and ML model setup (Completed)
Training and initial testing of ML models (Completed)
Automation of input data prediction via GEE/Colab (To do)
Continuous irrigation forecast generation and output delivery (To do)
Steps to a solution
The solution workflow begins by collecting and preprocessing key spectral indices derived from historical satellite datasets. These include Normalized Difference Vegetation Index (NDVI), Soil-Adjusted Vegetation Index (SAVI), Land Surface Temperature (LST), Land Use Land Cover (LULC), and Net Radiation (Rn) data. This includes the:
Dataset Preparation:
Extract temporal identifiers from each dataset.
Group datasets by matching dates across all indices and the target variable Evapotranspiration (ET).
Data pre-processing to clean datasets to remove NaN values and outliers for consistent temporal-spatial alignment.
Model Development:
Features are stacked into multi-channel tensors for CNN models (e.g., 5 input channels for NDVI, SAVI, LST, Rn, and LULC).
For Random Forest models, the same data is flattened into tabular format with each pixel representing a row.
Convolutional Neural Network (CNN):
A deep CNN model is trained with 5 layers including convolution (Conv2D) and Batch Normalization, activated using ReLU functions.
The final layer outputs a single channel of predicted Evapotranspiration (crop water requirement) for each crop pixel by pixel.
Random Forest Ensemble:
A bootstrapped ensemble of Random Forest regressors is trained on flattened data.
Each model votes on ET prediction, and the final output is an average of these predictions
Results
Initial model testing achieved accurate crop water requirement estimation using CNN and ML. Results indicated high R² values (e.g., NDVI = 0.81, SAVI = 0.81, Net Radiation = 0.83, LST = 0.78). A 7-day irrigation forecast was generated for rice, providing actionable advisories. The model testing phase has been completed and is now in the process of being brought into a continuous irrigation advisory system to generate crop driven irrigation forecasts.
The irrigation demand forecasting model was validated across two cropping seasons with Kharif (June 2024) and Rabi (February 2024), using observed evapotranspiration (ET) from PySEBAL and flux tower data. During the Kharif season, CNN predictions closely aligned with observed ET for rice (CNN: 6.798 mm/day vs. PySEBAL: 6.370 mm/day; Flux Tower: 6.99 mm/day), while RF and XGB models showed moderate underestimations.
Similarly, in the Rabi season, wheat ET prediction by CNN (2.041 mm/day) was close to the flux tower estimate (1.86 mm/day), with XGB and RF providing slightly conservative outputs. Across both seasons, CNN consistently performed better in spatial alignment and magnitude, demonstrating its robustness in capturing seasonal irrigation demand variations across diverse crops like maize, potato, guava, and citrus orchards.
To address the challenge of water security in Bahrain, this solution integrates space-based technologies and geospatial analysis to identify and monitor potential water resources, particularly shallow groundwater. The methodology involves the use of satellite-derived datasets and terrain modelling tools to analyse hydrological behaviour, soil moisture, and elevation-based drainage characteristics.
Three main data sources were incorporated into the solution:
GRACE (Gravity Recovery and Climate Experiment) data is used to assess changes in terrestrial water storage at the regional scale by detecting gravity anomalies related to mass variations in groundwater. GRACE data is retrieved and visualised through platforms such as Google Earth Engine and ArcGIS Pro, enabling temporal monitoring of water resources.
HAND (Height Above Nearest Drainage) modelling was employed to identify topographic wetness and assess the hydrological potential of the landscape. HAND normalises elevation relative to the nearest drainage, highlighting areas where water is more likely to accumulate or infiltrate. This method supports the identification of suitable zones for groundwater recharge, such as infiltration basins or artificial wetlands, especially in an arid environment like Bahrain. The HAND model was derived using the GLO-30 Copernicus DEM (2023_1 DGED version), processed through the TerraHidro platform, and included the generation of essential layers such as flow direction (D8), contributing area (D8CA), slope, and drainage networks with thresholds of 10, 100, and 300 pixels.
Soil moisture analysis was conducted using two approaches:
SAR (Synthetic Aperture Radar) data from the Sentinel-1 constellation, which provides all-weather, day-and-night measurements of surface moisture conditions.
Optical-based soil moisture estimation, calculated from Landsat-8 imagery using vegetation and thermal indices (e.g., Normalized Difference Vegetation Index (NDVI), Land Surface Temperature (LST)). This dual approach allows for consistent monitoring of surface moisture, which is crucial for assessing recharge potential and supporting irrigation planning.
Together, these tools provide a multi-faceted view of Bahrain's hydrological landscape, enabling decision-makers to strategically identify areas with groundwater potential and implement more sustainable water resource management practices.
Solution requirements
Gravity Recovery and Climate Experiment (GRACE)
GRACE is a joint mission by the National Aeronautics and Space Administration (NASA) and the German Aerospace Center (DLR) to measure Earth's gravity field anomalies from its launch in March 2002 to the end of its mission in October 2017. The GRACE Follow-On (GRACE-FO) is a continuation of the mission launched in May 2018. GRACE provides information on how mass is distributed and is varied over time through its detection of gravity anomalies. Because of this, a significant application of GRACE is groundwater anomalies detection. Hence, GRACE data has been explored as a solution for this challenge.
Two software platforms have been utilised to download and visualise GRACE data for Bahrain:
Google Earth Engine (GEE): A cloud-based platform that facilitates remote sensing analysis with a large catalogue of satellite imagery and geospatial datasets. The platform is free for academic and research purposes.
QGIS: A desktop application that allows the exploration, analysis and visualisation of geospatial data. This application is open source.
Height Above Nearest Drainage (HAND)
The Height Above Nearest Drainage (HAND) is a terrain model that normalises elevation data relative to the local drainage network, offering a hydrologically meaningful representation of the landscape. By calculating the vertical distance between each point on the terrain and the nearest drainage channel, HAND allows for the identification of topographic wetness zones and the classification of soil water environments. It has shown strong correlation with water table depth and has been effectively validated in various catchments, particularly in the Amazon region. The HAND model supports physically based hydrological modelling and has broad applicability in areas such as flood risk assessment, soil moisture mapping, and groundwater dynamics, using only remote sensing-derived topographic data as input.
Soil moisture using Synthetic Aperture Radar (SAR) imagery
SAR data from Sentinel-1 constellation was used to generate relative soil moisture values. Seninel-1 is a radar-based satellite which acquires data with 6 days repeat cycle, and is neither affected by clouds, weather nor time of the day. Being a dual-polarimetric platform, it acquires data in VV (Vertical-transmit and Vertical received) polarization and VH (Vertical-transmit and Horizontal received) polarization. The data was analysed in GEE.
Soil moisture using multispectral and thermal imagery (Optical)
The data utilised to detect soil moisture are satellite imagery from Landsat-8 downloaded through GEE. Landsat-8 provides multispectral and thermal satellite imagery with 16 days repeat cycle. The specific bands required to calculate soil moisture index are the red, near-infrared bands and thermal infrared bands.
Solution outline and steps
GRACE
Figure 1 illustrates the steps taken to extract the recent GRACE Monthly Mass Grids Version 04 - Global Mascon (CRI Filtered) Dataset from GEE.
Figure 1. Download steps for GRACE Data
HAND
The elevation data downloaded and processed for the region of interest were derived from the GLO-30 dataset. The Copernicus DEM, a Digital Surface Model (DSM), represents the Earth's surface, including features such as buildings, vegetation, and infrastructure. This DSM is based on the WorldDEM product, which has undergone extensive editing to ensure the flattening of water bodies, consistent river flow representation, and correction of terrain anomalies, including shorelines, coastlines, and features like airports. The WorldDEM itself was generated using radar satellite data from the TanDEM-X mission, a Public Private Partnership between the German Aerospace Centre (DLR) and Airbus Defence and Space. The GLO-30 data used in this work corresponds to the 2023_1 version of the Defence Gridded Elevation Data (DGED), provided via ESA’s https PRISM service and made accessible through OpenTopography.
The following products were processed using the TerraHidro software from the GLO-30 dataset: removepits.tif, d8.tif, d8ca.tif, slope.tif, drainage_10.tif, drainage_100.tif, and drainage_300.tif, as well as the HAND-derived products hand_10.tif, hand_100.tif, and hand_300.tif. Each product has a specific role in hydrological modeling:
removepits: This process modifies the original Digital Elevation Model (DEM) to eliminate depressions or pits that are not hydrologically realistic, ensuring that every cell has a defined downstream flow direction.
d8: The D8 (Deterministic 8) flow direction model calculates the steepest descent path from each pixel to one of its eight neighbors, indicating the primary direction of surface water flow.
d8ca: The D8 Contributing Area represents the number of upstream cells that contribute flow to each cell, allowing the identification of areas of potential accumulation and drainage.
slope: This product calculates the slope of the terrain in degrees, essential for understanding runoff velocity and erosion potential.
drainage_10, drainage_100, and drainage_300: These are drainage networks derived from the D8 contributing area, using threshold values of 10, 100, and 300 pixels, 0.9ha, 9ha and 27ha, respectively. They represent streams formed when the contributing area exceeds the specified number of pixels, with higher thresholds resulting in more generalised drainage networks.
From these products, the following HAND (Height Above Nearest Drainage) models were generated:
hand_10, hand_100, and hand_300: These datasets represent the vertical distance (in meters) from each pixel to the nearest drainage cell identified in the corresponding drainage network (with thresholds of 10, 100, and 300 pixels, respectively). These HAND maps are used to characterise terrain wetness, identify flood-prone areas, and support soil moisture and hydrological modeling.
Several steps were executed to derive the mean soil moisture conditions over the study area between 2017 and 2024. A step-by-step guide is shown in Figure 2. The values of soil moisture estimated is relative to the maximum soil moisture recorded in the region such that the wettest will be the maximum and the driest will be the minimum. These are used to normalise the final output into values between 0 and 1 where 0 is the driest and 1 is the wettest.
Figure 2. Processing steps for SAR soil moisture
Soil moisture (Optical)
Similar to the soil moisture calculation with SAR, an average of the soil moisture from 2017 to 2024 has been derived. The interrelations between the derived vegetation through the Normalized Difference Vegetation Index (NDVI) as well as Land Surface Temperature (LST) have been the basis for generating the soil moisture map. Figure 3 demonstrates the steps followed to generate optical soil moisture.
Figure 3. Processing steps for optical soil moisture
Shallow groundwater locations/recharge areas
To estimate potential suitable locations for shallow groundwater or groundwater rechange, the results from the HAND, SAR and optical soil moisture have been aggregated to formulate a final classification map. To perform this, the following has been done:
Classification of HAND, SAR and optical soil moisture results to ranges from 1-5, with 5 being the most suitable region based on the related values.
Spatial modelling of these three classifications to formulate a final suitability value from 1-5 with 5 being the most suitable region overall. HAND has been given a weightage of 50 per cent while SAR and optical soil moisture have been given a weightage of 25 per cent each to represent 50 per cent overall for soil moisture.
Map generation
Different maps have been generated for each component of this solution (HAND, SAR soil moisture, optical soil moisture, shallow groundwater locations/recharge areas). The subsequent steps illustrate the steps needed to develop the maps for this solution:
A basemap is added to the map for visualisation purposes. This is done through using the QGIS plugin called QuickMapServices. To install plugins, go to the Plugins tab and select Manage and Install Plugins.
Figure 4. Map generation - Step 1
In the search box of the Plugins window, search for QuickMapServices and install the plugin.
Figure 5. Map generation - Step 2
The plugin logo should appear in the QGIS panel. Click on the logo for Search QMS Panel. This label would appear if you hovered over the logo.
Figure 6. Map generation - Step 3
In the Search QMS Panel on the right, search for Google Satellite and add the basemap. It should appear in the list of layers.
Figure 7. Map generation - Step 4
Now we have a base layer that we can place our analysis on top of. Add the layer to the QGIS project if it is not already added. This can be done through drag and drop.
Figure 8. Map generation - Step 5
Right click on the layer and select Properties to adjust visualisation parameters.
Figure 9. Map generation - Step 6
In the Layer Properties window, click on Symbology and discover the most appropriate visualisation method for the data layer. This is an example for the set classifications for the HAND.
Figure 10. Map generation - Step 7
Once the layer visualisation has been set, the map layout can be generated. Go to Project > New Print Layout and name the layout.
Figure 11. Map generation - Step 8
Figure 12. Map generation - Step 8
In the Layout window, items such as the layers map, legend, scales can be added. This is accessed through the Add Item tab.
Figure 13. Map generation - Step 9
The items added to the map can then be moved and arranged by selecting the Edit tab then either Select/Move Content to move the locations of the specific content or Move Content to move the position/scale of the map.
Figure 14. Map generation - Step 10
Each item’s properties such as size, colour and fonts can also be edited in the Item Properties panel in the right.
Figure 15. Map generation - Step 11
The final generated layout is then exported in the desired format: png, pdf or svg. This is achieved through clicking on the Layout tab.
Figure 16. Map generation - Step 12
Results and maps
GRACE
The GRACE data has been downloaded and analysed through GEE. The main limitation of this dataset is its course resolution of 55.6 km2 as downloaded from the platform. This is due to the small geographical area of Bahrain at around 800 km2, causing water storage monitoring in specific locations to be a difficult task. Figure 17 demonstrates the span of GRACE data relative to the area of Bahrain.
Figure 17.GRACE Mascon- 2002 to 2024 Bahrain
HAND
The HAND model shown in the figure 18 provides valuable insights for addressing water scarcity in Bahrain. The low-lying areas highlighted in blue indicate regions where water tends to accumulate or water table is relatively shallow, suggesting potential zones for managed aquifer recharge (MAR) or stormwater harvesting. These areas could be prioritised for infiltration basins, recharging wells, or constructed wetlands to enhance groundwater storage. Conversely, the higher elevation zones in grey are less likely to retain surface water but could be strategically used for runoff collection and diversion to recharge areas. Given Bahrain’s arid climate and dependence on non-conventional water sources, integrating HAND-based terrain analysis into water resource planning can support more resilient, localised, and efficient water management strategies, particularly in optimising land use for recharge, storage, and flood mitigation purposes.
Figure 18. HAND results map
Soil moisture (SAR)
Figure 19 shows the mean soil moisture values of different regions of Bahrain. The southern regions seem to be drier while most central regions are wet. The analysis excluded urban regions.
Figure 19. SAR soil moisture results map
Soil moisture (Optical)
Figure 20 illustrates the soil moisture map with optical imagery for Bahrain. The results here highlight the northern west regions with high soil moisture values and the central, southern regions as dry with some specific location in the central and southern regions as wet.
Figure 20. Optical soil moisture results map
Shallow groundwater locations/recharge areas
Through Figure 5, the combinations of HAND, SAR and optical soil moisture has yielded to the potential locations for shallow groundwater locations/recharge areas. The areas highlighted in red represent the locations with highest potential.
Figure 21. Shallow groundwater locations/recharge areas results map
Solution impact
With the establishment of a methodology that identifies locations of shallow groundwater or recharge, significant information is being derived about the hydrological state of the country. This importance is placed due to the lack of remote sensing data that enables direct measurement of groundwater in the area. Hence the information extracted from this methodology can be initially integrated with sample in-situ data to calibrate the model; and then, be relied on solely for future measurements. Additionally, with the country’s rigorous focus on addressing groundwater scarcity, this type of information can greatly support decision-making when it comes to the formulation and execution of different projects and policies related to this matter.
Future work
To enhance the accuracy, applicability, and long-term impact of this solution in addressing water scarcity in Bahrain, several future developments are proposed:
Integration of additional remote sensing products: Incorporate higher-resolution satellite data to improve spatial resolution in soil moisture and elevation analyses, enabling finer-scale hydrological modeling and more localised identification of recharge zones. Moreover, the inclusion of land cover and geological characteristics can enhance the spatial modelling conducted.
Validation with in-situ data: Collaborate with local water authorities to collect and integrate ground-truth data such as groundwater levels, soil profiles, and well yields to validate and calibrate the HAND model and soil moisture outputs. This is also vital to assess the suitable weightage and classification for spatial modelling to be done to combine all three products generated.
Development of a Decision Support System (DSS): Create an interactive platform or dashboard that integrates HAND, GRACE, and soil moisture maps to assist policymakers in identifying priority areas for groundwater recharge, stormwater harvesting, and drought preparedness.
Temporal analysis and trend monitoring: Implement time-series analyses of GRACE and soil moisture data to detect trends, seasonal variations, and anomalies in water availability, supporting early warning systems and long-term planning.
Hydrological modelling coupling: Link HAND-derived terrain data with physically based hydrological models (e.g., SWAT, DHSVM) to simulate runoff, infiltration, and recharge scenarios under different land use and climate conditions.
Community engagement and capacity building: Conduct training workshops and knowledge-sharing activities with national institutions and stakeholders to build local capacity in geospatial water resource monitoring using open-source and space-based tools.
By pursuing these developments, the solution can evolve into a comprehensive and replicable model for sustainable groundwater resource management in water-scarce regions worldwide.
Relevant publications
Related space-based solutions
Sources
Nobre, A. D., Cuartas, L. A., Hodnett, M., Rennó, C. D., Rodrigues, G., Silveira, A., Waterloo, M., & Saleska, S. “Height Above the Nearest Drainage – a hydrologically relevant new terrain model.” Journal of Hydrology 404, no. 1–2 (2011): 13–29. https://doi.org/10.1016/j.jhydrol.2011.03.051.