Desert flash floods form hyperpycnal flows in the coral-rich Gulf of Aqaba, Red Sea

T. Katz, H. Ginat, G. Eyal, Z. Steiner, Y. Braun, S. Shalev, B. N. Goodman-Tchernov

Research output: Contribution to journalArticlepeer-review

81 Scopus citations

Abstract

Running rivers are very scarce in globally distributed hyperarid and arid coastlines (~28,000 km worldwide), and it is ephemeral rivers that carry most terrestrial sediment into the sea in these regions. However, there is very little information regarding the contribution of terrestrial sediment and dynamics of transport of sediment that enter marine basins from these rivers. One hyperarid region, the Gulf of Aqaba received an exceptional number of flashflood events during the winter of 2012-2013. The results illustrate, for the first time, how the high volume of flashflood sediment influences the distribution of coral reefs; dwarfs the contribution of airborne dust; elevates floodwater densities to produce hyperpycnal flows, despite highest ocean salinities; and is subsequently transported to the deep basin where it may be preserved as a climate archive.

Original languageEnglish
Pages (from-to)87-98
Number of pages12
JournalEarth and Planetary Science Letters
Volume417
DOIs
StatePublished - 1 May 2015
Externally publishedYes

Bibliographical note

Publisher Copyright:
© 2015 Elsevier B.V.

Keywords

  • Ephemeral-rivers
  • Flashfloods
  • Hyperarid
  • Hyperpycnal
  • Sediments
  • Turbidity currents

Fingerprint

Dive into the research topics of 'Desert flash floods form hyperpycnal flows in the coral-rich Gulf of Aqaba, Red Sea'. Together they form a unique fingerprint.

Cite this