<p>Recent research published in <strong>Current Science</strong> reveals that flood hazard assessments for <strong>Uttarakhand</strong> have consistently undervalued the danger to towns and villages because they rely on long‑term average rainfall rather than the extreme downpours that trigger disasters.</p>
<h3>Key Developments</h3>
<ul>
<li>Analysis of flood hazard zones for the period <strong>2017‑2021</strong> shows a marked rise in areas classified as ‘high’ or ‘severe’ hazard, with <strong>2021</strong> recording the largest extent of high‑hazard land.</li>
<li>More than <strong>90 %</strong> of the state fell within moderate or high‑hazard categories across all years studied.</li>
<li>Researchers from <strong>Malaviya National Institute of Technology (MNIT), Jaipur</strong> used a <span class="key-term" data-definition="Geographic Information System (GIS) — A digital platform for capturing, storing, analysing and visualising spatial data; essential for planning and disaster management (GS2: Polity, GS3: Economy)">GIS</span> model that combined six factors—elevation, slope, drainage density, topographic wetness, land use and rainfall—to map flood risk.</li>
<li>When the model employed the highest annual rainfall recorded in a year, severe and high‑hazard zones expanded dramatically; using three‑decade averages produced a misleadingly smaller risk area.</li>
</ul>
<h3>Important Facts</h3>
<p>The six‑factor weighting gave the greatest importance to <span class="key-term" data-definition="Slope — The steepness of terrain; steeper slopes accelerate runoff and increase flood potential (GS3: Environment)">slope</span>, <span class="key-term" data-definition="Elevation — Height above sea level; lower elevations often lie in floodplains (GS3: Environment)">elevation</span> and <span class="key-term" data-definition="Rainfall — Precipitation amount; extreme rainfall events are becoming more frequent in the Himalayas due to climate change (GS3: Environment)">rainfall</span>. Land‑use change, drainage density and topographic wetness were treated as secondary factors.</p>
<p>Historical catastrophes such as the <strong>Malpa landslide (1998)</strong>, the <strong>Kedarnath disaster (2013)</strong>—where Uttarakhand received <strong>375 %</strong> of its benchmark monsoon rainfall—and the <strong>Chamoli flood (2021)</strong> underscore the growing vulnerability. Climate scientists link the rising frequency of <span class="key-term" data-definition="Cloudburst — A sudden, intense rainfall event that can cause flash floods, especially in mountainous regions (GS3: Environment)">cloudbursts</span> and <span class="key-term" data-definition="Glacial lake outburst — A rapid release of water from a glacial lake, often leading to downstream flooding (GS3: Environment)">glacial lake outbursts</span> to a warming atmosphere.</p>
<p>Rapid urbanisation has expanded built‑up areas, reducing land’s capacity to absorb runoff and further aggravating flood risk