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Global-scale human impact on delta morphology has led to net land area gain

  • J H Nienhuis
  • , A D Ashton
  • , D A Edmonds
  • , A J F Hoitink
  • , A J Kettner
  • , J C Rowland
  • , T E Törnqvist
  • Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA, USA.
  • Department of Earth and Atmospheric Sciences, Indiana University, Bloomington, IN, USA.
  • Institute of Arctic and Alpine Research, University of Colorado, Boulder, CO, USA.
  • Earth & Environmental Sciences Division, Los Alamos National Laboratory, Los Alamos, NM, USA.
  • Department of Earth and Environmental Sciences, Tulane University, New Orleans, LA, USA.

Research output: Contribution to journalArticleAcademicpeer-review

Abstract

River deltas rank among the most economically and ecologically valuable environments on Earth. Even in the absence of sea-level rise, deltas are increasingly vulnerable to coastal hazards as declining sediment supply and climate change alter their sediment budget, affecting delta morphology and possibly leading to erosion1-3. However, the relationship between deltaic sediment budgets, oceanographic forces of waves and tides, and delta morphology has remained poorly quantified. Here we show how the morphology of about 11,000 coastal deltas worldwide, ranging from small bayhead deltas to mega-deltas, has been affected by river damming and deforestation. We introduce a model that shows that present-day delta morphology varies across a continuum between wave (about 80 per cent), tide (around 10 per cent) and river (about 10 per cent) dominance, but that most large deltas are tide- and river-dominated. Over the past 30 years, despite sea-level rise, deltas globally have experienced a net land gain of 54 ± 12 square kilometres per year (2 standard deviations), with the largest 1 per cent of deltas being responsible for 30 per cent of all net land area gains. Humans are a considerable driver of these net land gains-25 per cent of delta growth can be attributed to deforestation-induced increases in fluvial sediment supply. Yet for nearly 1,000 deltas, river damming4 has resulted in a severe (more than 50 per cent) reduction in anthropogenic sediment flux, forcing a collective loss of 12 ± 3.5 square kilometres per year (2 standard deviations) of deltaic land. Not all deltas lose land in response to river damming: deltas transitioning towards tide dominance are currently gaining land, probably through channel infilling. With expected accelerated sea-level rise5, however, recent land gains are unlikely to be sustained throughout the twenty-first century. Understanding the redistribution of sediments by waves and tides will be critical for successfully predicting human-driven change to deltas, both locally and globally.

Original languageEnglish
Pages (from-to)514-518
Number of pages5
JournalNature
Volume577
Issue number7791
DOIs
Publication statusPublished - Jan 2020

UN SDGs

This output contributes to the following UN Sustainable Development Goals (SDGs)

  1. SDG 13 - Climate Action
    SDG 13 Climate Action
  2. SDG 15 - Life on Land
    SDG 15 Life on Land

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