KAZA Surface Water Maps


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Created: Oct 29, 2025 at 8:36 p.m. (UTC)
Last updated: Jul 28, 2026 at 3:12 p.m. (UTC)
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Abstract

Reliable freshwater access drives terrestrial wildlife movements and habitat use globally. The small, rain-fed seasonal pools critical for dryland wildlife persistence are vulnerable to rising temperatures and unstable precipitation regimes projected under climate change. In southern Africa, which is expected to warm rapidly by 2100, the drying and disappearance of surface water may cause a breakdown in seasonal migrations of large, area-sensitive, and water-dependent wildlife species. Furthermore, the disappearance of ephemeral water may concentrate wildlife around remaining surface water, increasing resource competition and human-wildlife conflict. An accurate understanding of the dynamics and drivers of seasonal surface water will therefore be crucial to wildlife and human health as climate change intensifies.

Here, we present a framework and empirical analysis of fine-scale surface water mapping in the Kavango Zambezi Transfrontier Conservation Area (KAZA), the world's largest terrestrial conservation area (520,000km2). From 2019-2025, we implemented Otsu thresholding on median Automated Water Extraction Index Sentinel-2 MSI imagery (10m), creating >35 quasi-monthly KAZA-wide Ephemeral Surface Water (ESW) rasters (mean accuracy 87%, compared to 50% for a 30m Global Surface Water (GSW) product). Low wet season (November-May) rainfall drove led to low surface water fill from February-May, especially after multiple drought years (2023-2024), suggesting a critically vulnerable time for water-dependent wildlife.

Finally, we assessed the applicability of our ESW map for wildlife movement analyses. African savanna elephant (Loxodonta africana) are known to visit water approximately every 48 hours; a useful water map should reflect this dependence. We calculated water visitation rates using GPS data from 27 individual elephant and a threshold distance of T = 200m, and found that 99% of GPS tracks maintained ESW visitation rates under 48 hours, compared to only 29% of tracks for GSW visitation. These results were robust when T was varied, and ESW similarly outperformed random controls and several other water products, making ESW an effective proxy for actual water use in animal movement models. As climate change threatens seasonally ephemeral surface water, fine-resolution tools such as ESW will help conservation scientists and managers to understand and predict the drivers of wildlife movements at the scale of wildlife needs.

Subject Keywords

Coverage

Spatial

Coordinate System/Geographic Projection:
WGS84 EPSG:4326
Coordinate Units:
['Decimal degrees']
North Latitude
-13.5138°
East Longitude
32.5535°
South Latitude
-23.5637°
West Longitude
15.2830°

Temporal

Start Date:
End Date:

Collection Contents

Add Title Type Owners Sharing Status Remove
KAZA Surface Water GEE Workflow Resource Maggie Swift Public & Shareable
KAZA Validation Data Resource Maggie Swift Public & Shareable
Ephemeral Surface Water (ESW) regional files Resource Maggie Swift Public & Shareable
Maximum Water Fill (MWF) Rasters Resource Maggie Swift Public & Shareable
Ephemeral Surface Water Recurrence (ESWr) Resource Maggie Swift Public & Shareable

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Credits

Funding Agencies

This resource was created using funding from the following sources:
Agency Name Award Title Award Number
WWF-US None None

Contributors

People or Organizations that contributed technically, materially, financially, or provided general support for the creation of the resource's content but are not considered authors.

Name Organization Address Phone Author Identifiers
Robin Naidoo WWF-US
Piet Beytell MEFT
Anna Songhurst Ecoexist Trust
Graham McCulloch Ecoexist Trust

How to Cite

Swift, M. (2026). KAZA Surface Water Maps, HydroShare, http://www.hydroshare.org/resource/8d974079c9f146cfa25aaeeab7a8a342

This resource is shared under the Creative Commons Attribution CC BY.

http://creativecommons.org/licenses/by/4.0/
CC-BY

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