Related Experiment Video
Updated: May 23, 2025

Measuring the Structure, Composition, and Change of Underwater Environments with Large-area Imaging
Published on: April 18, 2025
ROBIN: Reference observatory of basins for international hydrological climate change detection
S Turner1, J Hannaford2,3, L J Barker2
1UK Centre for Ecology & Hydrology, Wallingford, United Kingdom. stetur@ceh.ac.uk.
Abstract:
Human-induced warming is modifying the water cycle. Adaptation to posed threats requires an understanding of hydrological responses to climate variability. Whilst these can be computationally modelled, observed streamflow data is essential for constraining models, and understanding and quantifying emerging trends in the water cycle. To date, the identification of such trends at the global scale has been hindered by data limitations - in particular, the prevalence of direct human influences on streamflow which can obscure climate-driven variability. By removing these influences, trends in streamflow data can be more confidently attributed to climate variability. Here we describe the Reference Observatory of Basins for INternational hydrological climate change detection (ROBIN) - the first iteration of a global network of streamflow data from national reference hydrological networks (RHNs) - comprised of catchments which are near-natural or have limited human influences. This collaboration has established a freely available global RHN dataset of over 3,000 catchments and code libraries, which can be used to underpin new science endeavours and advance change detection studies to support international climate policy and adaptation.
Related Concept Videos
Global Climate Change
Precipitation Gravimetry
In determining nickel by gravimetric analysis, a precipitant of ethanolic dimethylglyoxime is added to a hot nickel salt solution. This is quickly followed by the dropwise addition of dilute ammonia solution until precipitation occurs. A...
Precipitation and Co-precipitation
The Water Cycle
Precipitation Processes
Isochoric and Isobaric Processes
Suppose 1000 g of water is heated from 40...

