<HashMap><database>biostudies-literature</database><scores/><additional><omics_type>Unknown</omics_type><volume>12(1)</volume><submitter>Warrick JA</submitter><pubmed_abstract>Wildfire and post-fire rainfall have resounding effects on hillslope processes and sediment yields of mountainous landscapes. Yet, it remains unclear how fire-flood sequences influence downstream coastal littoral systems. It is timely to examine terrestrial-coastal connections because climate change is increasing the frequency, size, and intensity of wildfires, altering precipitation rates, and accelerating sea-level rise; and these factors can be understood as contrasting accretionary and erosive agents for coastal systems. Here we provide new satellite-derived shoreline measurements of Big Sur, California and show how river sediment discharge significantly influenced shoreline positions during the past several decades. A 2016 wildfire followed by record precipitation increased sediment discharge in the Big Sur River and resulted in almost half of the total river sediment load of the past 50 years (~ 2.2 of ~ 4.8 Mt). Roughly 30% of this river sediment was inferred to be littoral-grade sand and was incorporated into the littoral cell, causing the widest beaches in the 37-year satellite record and spreading downcoast over timescales of years. Hence, the impact of fire-flood events on coastal sediment budgets may be substantial, and these impacts may increase with time considering projected intensification of wildfires and extreme rain events under global warming.</pubmed_abstract><journal>Scientific reports</journal><pagination>3848</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC8907308</full_dataset_link><repository>biostudies-literature</repository><pubmed_title>Fire (plus) flood (equals) beach: coastal response to an exceptional river sediment discharge event.</pubmed_title><pmcid>PMC8907308</pmcid><pubmed_authors>Warrick JA</pubmed_authors><pubmed_authors>Vitousek S</pubmed_authors><pubmed_authors>Vos K</pubmed_authors><pubmed_authors>East AE</pubmed_authors></additional><is_claimable>false</is_claimable><name>Fire (plus) flood (equals) beach: coastal response to an exceptional river sediment discharge event.</name><description>Wildfire and post-fire rainfall have resounding effects on hillslope processes and sediment yields of mountainous landscapes. Yet, it remains unclear how fire-flood sequences influence downstream coastal littoral systems. It is timely to examine terrestrial-coastal connections because climate change is increasing the frequency, size, and intensity of wildfires, altering precipitation rates, and accelerating sea-level rise; and these factors can be understood as contrasting accretionary and erosive agents for coastal systems. Here we provide new satellite-derived shoreline measurements of Big Sur, California and show how river sediment discharge significantly influenced shoreline positions during the past several decades. A 2016 wildfire followed by record precipitation increased sediment discharge in the Big Sur River and resulted in almost half of the total river sediment load of the past 50 years (~ 2.2 of ~ 4.8 Mt). Roughly 30% of this river sediment was inferred to be littoral-grade sand and was incorporated into the littoral cell, causing the widest beaches in the 37-year satellite record and spreading downcoast over timescales of years. Hence, the impact of fire-flood events on coastal sediment budgets may be substantial, and these impacts may increase with time considering projected intensification of wildfires and extreme rain events under global warming.</description><dates><release>2022-01-01T00:00:00Z</release><publication>2022 Mar</publication><modification>2025-04-29T11:01:16.181Z</modification><creation>2025-04-06T19:50:30.563Z</creation></dates><accession>S-EPMC8907308</accession><cross_references><pubmed>35264600</pubmed><doi>10.1038/s41598-022-07209-0</doi></cross_references></HashMap>