Downward particle fluxes of biogenic matter and Saharan dust across the equatorial North Atlantic

التفاصيل البيبلوغرافية
العنوان: Downward particle fluxes of biogenic matter and Saharan dust across the equatorial North Atlantic
المؤلفون: Rick Hennekam, Jan-Berend W Stuut, Michèlle van der Does, Stefan Schouten, Geert-Jan A Brummer, Dirk Jong, Laura F Korte, Catarina Guerreiro, Johannes A van Hateren, Chris I Munday
المساهمون: Earth and Climate
المصدر: Korte, L F, Brummer, G J A, Van Der Does, M, Guerreiro, C V, Hennekam, R, Van Hateren, J A, Jong, DI, Munday, C I, Schouten, S & Stuut, J B W 2017, ' Downward particle fluxes of biogenic matter and Saharan dust across the equatorial North Atlantic ', Atmospheric Chemistry and Physics, vol. 17, no. 9, pp. 6023-6040 . https://doi.org/10.5194/acp-17-6023-2017
Atmospheric Chemistry and Physics, 17(9), 6023-6040. European Geosciences Union
Atmospheric Chemistry and Physics, Vol 17, Iss 9, Pp 6023-6040 (2017)
بيانات النشر: Copernicus GmbH, 2017.
سنة النشر: 2017
مصطلحات موضوعية: Atmospheric Science, 010504 meteorology & atmospheric sciences, Biogenic silica, Seasonality, Mineral dust, 010502 geochemistry & geophysics, medicine.disease, 01 natural sciences, Deep sea, lcsh:QC1-999, Deposition (geology), lcsh:Chemistry, Oceanography, lcsh:QD1-999, 13. Climate action, Sediment trap, medicine, Spatial variability, SDG 14 - Life Below Water, Transect, lcsh:Physics, Geology, 0105 earth and related environmental sciences
الوصف: Massive amounts of Saharan dust are blown from the coast of northern Africa across the Atlantic Ocean towards the Americas each year. This dust has, depending on its chemistry, direct and indirect effects on global climate which include reflection and absorption of solar radiation as well as transport and deposition of nutrients and metals fertilizing both ocean and land. To determine the temporal and spatial variability of Saharan dust transport and deposition and their marine environmental effects across the equatorial North Atlantic Ocean, we have set up a monitoring experiment using deep-ocean sediment traps as well as land-based dust collectors. The sediment traps were deployed at five ocean sites along a transatlantic transect between north-west Africa and the Caribbean along 12° N, in a downwind extension of the land-based dust collectors placed at 19° N on the Mauritanian coast in Iouîk. In this paper, we lay out the setup of the monitoring experiment and present the particle fluxes from sediment trap sampling over 24 continuous and synchronized intervals from October 2012 through to November 2013. We establish the temporal distribution of the particle fluxes deposited in the Atlantic and compare chemical compositions with the land-based dust collectors propagating to the downwind sediment trap sites, and with satellite observations of Saharan dust outbreaks. First-year results show that the total mass fluxes in the ocean are highest at the sampling sites in the east and west, closest to the African continent and the Caribbean, respectively. Element ratios reveal that the lithogenic particles deposited nearest to Africa are most similar in composition to the Saharan dust collected in Iouîk. Downwind increasing Al, Fe and K contents suggest a downwind change in the mineralogical composition of Saharan dust and indicate an increasing contribution of clay minerals towards the west. In the westernmost Atlantic Ocean, admixture of re-suspended clay-sized sediments advected towards the deep sediment trap cannot be excluded. Seasonality is most prominent near both continents but generally weak, with mass fluxes dominated by calcium carbonate and clear seasonal maxima of biogenic silica towards the west. The monitoring experiment is now extended, with autonomous dust sampling buoys for better quantification of Saharan dust transport and deposition from source to sink and their impact on fertilization and carbon export to the deep ocean.
وصف الملف: application/pdf
تدمد: 1680-7324
1680-7316
URL الوصول: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::529f85c537d6dc1139998e300cf06600
https://doi.org/10.5194/acp-17-6023-2017
حقوق: OPEN
رقم الأكسشن: edsair.doi.dedup.....529f85c537d6dc1139998e300cf06600
قاعدة البيانات: OpenAIRE