Waves are an important agent in the construction, sha** and destruction of river deltas.
Notwithstanding the commonality of waves in oceans and seas, wave influence on deltas …

Future sea-level rise poses an existential threat for many river deltas, yet quantifying the
effect of sea-level changes on these coastal landforms remains a challenge. Sea-level …

The morphologies of the world's deltas are thought to be determined by river discharge, tidal
range and wave action. More recently, sea-level rise, and human engineering have been …

Climate, tectonics, and life influence the flux and caliber of sediment transported across
Earth's surface. These environmental conditions can leave behind imprints in the Earth's …

Accelerating sea‐level rise and decreasing riverine sediment supply are widely considered
to lead to global losses of deltaic marshes and their valuable ecosystem services. However …

Sediment flux from rivers to oceans is the fundamental driver of fluvio‐deltaic
morphodynamics and continental margin sedimentation, yet sediment transport across the …

Where rivers near the coastline, the receiving basin begins to influence flow, and gradually
varied, nonuniform flow conditions arise. The section of the river affected by nonuniform flow …

There is a pressing need to understand how different delta morphologies arise because
morphology determines a delta's ecologic structure, resilience to relative sea‐level rise, and …

The Jezero crater open-basin lake contains two well-exposed fluvial sedimentary deposits
formed early in martian history. Here, we examine the geometry and architecture of the …

At a global scale, delta morphologies are subject to rapid change as a result of direct and
indirect effects of human activity. This jeopardizes the ecosystem services of deltas …