<?xml version="1.0" encoding="UTF-8"?><rss version="2.0"
	xmlns:content="http://purl.org/rss/1.0/modules/content/"
	xmlns:wfw="http://wellformedweb.org/CommentAPI/"
	xmlns:dc="http://purl.org/dc/elements/1.1/"
	xmlns:atom="http://www.w3.org/2005/Atom"
	xmlns:sy="http://purl.org/rss/1.0/modules/syndication/"
	xmlns:slash="http://purl.org/rss/1.0/modules/slash/"
	>

<channel>
	<title>hydrological modeling under climate scenarios &#8211; Science</title>
	<atom:link href="https://scienmag.com/tag/hydrological-modeling-under-climate-scenarios/feed/" rel="self" type="application/rss+xml" />
	<link>https://scienmag.com</link>
	<description></description>
	<lastBuildDate>Mon, 26 Oct 2026 21:59:40 +0000</lastBuildDate>
	<language>en-US</language>
	<sy:updatePeriod>
	hourly	</sy:updatePeriod>
	<sy:updateFrequency>
	1	</sy:updateFrequency>
	<generator>https://wordpress.org/?v=7.1.3</generator>

<image>
	<url>https://scienmag.com/wp-content/uploads/2024/07/cropped-scienmag_ico-32x32.jpg</url>
	<title>hydrological modeling under climate scenarios &#8211; Science</title>
	<link>https://scienmag.com</link>
	<width>32</width>
	<height>32</height>
</image> 
<site xmlns="com-wordpress:feed-additions:1">73899611</site>	<item>
		<title>Bias-corrected climate models sharpen Kulfo River streamflow projections</title>
		<link>https://scienmag.com/bias-corrected-climate-models-sharpen-kulfo-river-streamflow-projections/</link>
		
		<dc:creator><![CDATA[Violet Maxwell]]></dc:creator>
		<pubDate>Mon, 26 Oct 2026 21:59:40 +0000</pubDate>
				<category><![CDATA[Earth Science]]></category>
		<category><![CDATA[bias correction]]></category>
		<category><![CDATA[bias correction methods for climate data]]></category>
		<category><![CDATA[climate change]]></category>
		<category><![CDATA[climate change impact on river discharge]]></category>
		<category><![CDATA[Climate model bias correction]]></category>
		<category><![CDATA[climate-driven flood and drought assessment]]></category>
		<category><![CDATA[CMIP6]]></category>
		<category><![CDATA[CMIP6 climate projections]]></category>
		<category><![CDATA[Ethiopia]]></category>
		<category><![CDATA[flood risk]]></category>
		<category><![CDATA[future water availability in data-scarce regions]]></category>
		<category><![CDATA[hydrological modeling under climate scenarios]]></category>
		<category><![CDATA[hydrology]]></category>
		<category><![CDATA[Kulfo River]]></category>
		<category><![CDATA[learning]]></category>
		<category><![CDATA[machine]]></category>
		<category><![CDATA[machine learning in hydrology]]></category>
		<category><![CDATA[prediction uncertainty]]></category>
		<category><![CDATA[prediction uncertainty in climate-hydrology models]]></category>
		<category><![CDATA[Random Forest]]></category>
		<category><![CDATA[Random Forest streamflow prediction]]></category>
		<category><![CDATA[streamflow forecasting in Ethiopia]]></category>
		<category><![CDATA[streamflow projection]]></category>
		<category><![CDATA[water resource management in Rift Valley]]></category>
		<guid isPermaLink="false">https://scienmag.com/?p=345058</guid>

					<description><![CDATA[A study combining bias-corrected CMIP6 projections and machine learning projected rising temperatures and declining Kulfo River discharge under three future-emissions scenarios by 2100.]]></description>
										<content:encoded><![CDATA[<p>A computational climate–hydrology–machine-learning study found that bias-corrected projections from 16 Coupled Model Intercomparison Project Phase 6 models could improve streamflow forecasting in Ethiopia’s data-scarce Kulfo watershed, while indicating rising temperatures and declining annual discharge under every future-emissions scenario examined. The researchers compared statistical and machine-learning bias-correction methods, assessed 10 machine-learning algorithms and quantified projection uncertainty with 95% prediction intervals. Random Forest performed best overall: the study reported up to a 92% reduction in precipitation root mean square error, a Nash–Sutcliffe Efficiency of 0.999 during calibration and 0.806 during validation for streamflow prediction.</p>
<p>The project focused on the Kulfo River in southern Ethiopia, part of the Rift Valley where limited observations complicate efforts to assess climate-driven changes in water availability and floods. The study assessed 16 CMIP6 models under the SSP1-2.6, SSP2-4.5 and SSP5-8.5 scenarios. It then combined bias-corrected climate projections with a hydrological model and machine-learning prediction methods, comparing approaches that might be useful where long, high-quality records are scarce. After correction, CNRM-ESM2-1 produced the strongest precipitation and minimum-temperature results, while CNRM-CM6-1 performed best for maximum temperature, according to the reported model comparison.</p>
<p>Future projections showed progressively greater streamflow reductions by 2100, with annual discharge estimated to decline by approximately 8.5% under SSP1-2.6, 13.9% under SSP2-4.5 and 20.7% under SSP5-8.5. Temperatures were projected to increase in each scenario. The study associated the declining discharge with increased evaporative demand and altered seasonal rainfall, including reduced summer flow and shifts in hydrological seasonality. Conformal prediction was used to express uncertainty around the modeled outcomes, and the analysis found that this uncertainty increased in the projections, particularly under the high-emissions SSP5-8.5 scenario. A separate non-stationary flood-frequency analysis also indicated significant changes in future flood characteristics, although the supplied findings do not provide specific change magnitudes for individual flood metrics.</p>
<p>The results suggest that careful correction of climate-model biases can make global climate ensembles more useful for hydrological assessment in a data-limited basin. The reported validation score of 0.806 is lower than the calibration value of 0.999, illustrating that performance outside the training period was not identical to performance during fitting. The authors also found that Random Forest outperformed the tested Long Short-Term Memory and other deep-learning methods, which they interpreted as evidence that simpler ensemble approaches may be suitable when training data are limited. This does not establish that Random Forest will perform equally well in other catchments: the findings are model- and study-specific, and the study’s scope was the Kulfo watershed rather than Ethiopian rivers generally. Even so, the integrated framework links climate-model bias correction, streamflow prediction, uncertainty estimation and flood assessment, offering a structured way to examine future water-resource risks where direct historical observations are sparse.</p>
<p><strong>Subject of Research:</strong> CMIP6 bias correction and machine-learning projections of streamflow change in Ethiopia’s Kulfo River watershed</p>
<p><strong>Article Title:</strong> Machine learning and bias corrected CMIP6 for improved streamflow prediction in the data-scarce Kulfo river, Ethiopia</p>
<p><strong>Article References:</strong> Ashagre, H. M., Goshime, D. W., Yersaw, B. T., &amp; Walle, M. A. (2026). Machine learning and bias corrected CMIP6 for improved streamflow prediction in the data-scarce Kulfo river, Ethiopia. <em>Discover Sustainability</em>. <a href="https://doi.org/10.1007/s43621-026-04724-2" rel="noopener noreferrer">https://doi.org/10.1007/s43621-026-04724-2</a></p>
<p><strong>Image Credits:</strong> AI Generated</p>
<p><strong>DOI:</strong> <a href="https://doi.org/10.1007/s43621-026-04724-2" rel="noopener noreferrer">10.1007/s43621-026-04724-2</a></p>
<p><strong>Keywords:</strong> Kulfo River, Ethiopia, CMIP6, streamflow projection, Random Forest, bias correction, climate change, hydrology, flood risk, prediction uncertainty, Machine, learning</p>
]]></content:encoded>
					
		
		
		<post-id xmlns="com-wordpress:feed-additions:1">345058</post-id>	</item>
	</channel>
</rss>
