Department of Physical Geography, Utrecht University, Utrecht, The Netherlands.
Department of Earth, Ocean, and Atmospheric Sciences, Florida State University, Tallahassee, FL, USA.
Nature. 2020 Jan;577(7791):514-518. doi: 10.1038/s41586-019-1905-9. Epub 2020 Jan 22.
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 erosion. 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 damming 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 rise, 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.
河流三角洲是地球上经济和生态价值最高的环境之一。即使海平面没有上升,由于沉积物供应减少和气候变化改变了它们的沉积物预算,三角洲也越来越容易受到沿海灾害的影响,影响三角洲的形态,并可能导致侵蚀。然而,三角洲的沉积物预算、波浪和潮汐的海洋学力量以及三角洲的形态之间的关系仍然没有得到很好的量化。在这里,我们展示了全球约 11000 个沿海三角洲的形态如何受到河流筑坝和森林砍伐的影响。我们引入了一个模型,表明当今三角洲的形态在波浪(约 80%)、潮汐(约 10%)和河流(约 10%)主导之间存在连续变化,但大多数大型三角洲是潮汐和河流主导的。在过去的 30 年里,尽管海平面上升,全球三角洲每年仍净增加 54±12 平方公里(2 个标准差),最大的 1%的三角洲占所有净陆地面积增加的 30%。人类是这些净陆地增加的一个重要驱动因素-三角洲增长的 25%可以归因于森林砍伐导致的河流沉积物供应增加。然而,对于近 1000 个三角洲来说,河流筑坝导致人为沉积物通量严重减少(超过 50%),迫使每年集体损失 12±3.5 平方公里(2 个标准差)的三角洲土地。并非所有三角洲都会因河流筑坝而失去土地:正在向潮汐主导转变的三角洲目前正在获得土地,可能是通过河道填充。然而,随着预计海平面加速上升,最近的土地收益在整个 21 世纪可能都无法持续。了解波浪和潮汐对沉积物的再分配对于成功预测人类驱动的三角洲变化至关重要,无论是在当地还是在全球范围内。