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N‐FOREWARNS: Regional Nowcasting of Surface Water Flooding With a 3‐h Lead Time Predictability Limit

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Published in:Meteorological Applications
Format: Online Article RSS Article
Published: 2026
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container_title Meteorological Applications
description
discipline_display Environmental Sciences
discipline_facet Environmental Sciences
format Online Article
RSS Article
genre Journal Article
id rss_article:24889
institution FRELIP
journal_source_facet Meteorological Applications
publishDate 2026
publishDateSort 2026
record_format rss_article
spellingShingle N‐FOREWARNS: Regional Nowcasting of Surface Water Flooding With a 3‐h Lead Time Predictability Limit
— — — — — — Meteorology
Climate & Atmospheric Sciences
Environmental Sciences
sub_discipline_display Climate & Atmospheric Sciences
sub_discipline_facet Climate & Atmospheric Sciences
subject_display — — — — — — Meteorology
Climate & Atmospheric Sciences
Environmental Sciences
— — — — — — Meteorology
Climate & Atmospheric Sciences
Environmental Sciences
subject_facet — — — — — — Meteorology
Climate & Atmospheric Sciences
Environmental Sciences
title N‐FOREWARNS: Regional Nowcasting of Surface Water Flooding With a 3‐h Lead Time Predictability Limit
title_auth N‐FOREWARNS: Regional Nowcasting of Surface Water Flooding With a 3‐h Lead Time Predictability Limit
title_full N‐FOREWARNS: Regional Nowcasting of Surface Water Flooding With a 3‐h Lead Time Predictability Limit
title_fullStr N‐FOREWARNS: Regional Nowcasting of Surface Water Flooding With a 3‐h Lead Time Predictability Limit
title_full_unstemmed N‐FOREWARNS: Regional Nowcasting of Surface Water Flooding With a 3‐h Lead Time Predictability Limit
title_short N‐FOREWARNS: Regional Nowcasting of Surface Water Flooding With a 3‐h Lead Time Predictability Limit
title_sort n‐forewarns: regional nowcasting of surface water flooding with a 3‐h lead time predictability limit
topic — — — — — — Meteorology
Climate & Atmospheric Sciences
Environmental Sciences
url https://rmets.onlinelibrary.wiley.com/doi/10.1002/met.70157?af=R