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dc.creatorStolle, Christian
dc.creatorRibas Ribas, Mariana
dc.creatorBadewien, Thomas H.
dc.creatorBarnes, Jonathan
dc.creatorCarpenter, Lucy J.
dc.creatorChance, Rosie
dc.creatorDamgaard, Lars Riis
dc.creatorDurán Quesada, Ana María
dc.creatorEngel, Anja
dc.creatorFrka, Sanja
dc.creatorGalgani, Luisa
dc.creatorGašparović, Blaženka
dc.creatorGerriets, Michaela
dc.creatorMustaffa, Nur Ili Hamizah
dc.creatorHerrmann, Hartmut
dc.creatorKallajoki, Liisa
dc.creatorPereira, Ryan
dc.creatorRadach, Franziska
dc.creatorRevsbech, Niels Peter
dc.creatorRickard, Philippa
dc.creatorSaint, Adam
dc.creatorSalter, Matthew
dc.creatorStriebel, Maren
dc.creatorTriesch, Nadja
dc.creatorUher, Guenther
dc.creatorUpstill Goddard, Robert C.
dc.creatorvan Pinxteren, Manuela
dc.creatorZäncker, Birthe
dc.creatorZieger, Paul
dc.creatorWurl, Oliver
dc.date.accessioned2019-12-03T16:47:07Z
dc.date.available2019-12-03T16:47:07Z
dc.date.issued2019
dc.identifier.citationhttps://journals.ametsoc.org/doi/abs/10.1175/BAMS-D-17-0329.1?mobileUi=0&es_ES
dc.identifier.issn1520-0477
dc.identifier.issn0003-0007
dc.identifier.urihttp://hdl.handle.net/10669/79969
dc.description.abstractThe sea-surface microlayer (SML) at the air-sea interface is < 1 mm deep but it is physically, chemically and biologically distinct from the underlying water and the atmosphere above. Wind-driven turbulence and solar radiation are important drivers of SML physical and biogeochemical properties. Given that the SML is involved in all ocean-atmosphere exchanges of mass and energy, its response to solar radiation, especially in relation to how it regulates the air-sea exchange of climate-relevant gases and aerosols, is surprisingly poorly characterised. MILAN (sea-surface MIcroLAyer at Night) was an international, multidisciplinary campaign designed to specifically address this issue. In spring 2017, we deployed diverse sampling platforms (research vessels, radio-controlled catamaran, free-drifting buoy) to study full diel cycles in the coastal North Sea SML and in underlying water, and installed a land based aerosol sampler. We also carried out concurrent ex situ experiments using several microsensors, a laboratory gas exchange tank, a solar simulator, and a sea spray simulation chamber. In this paper we outline the diversity of approaches employed and some initial results obtained during MILAN. Our observations of diel SML variability, e.g. the influence of changing solar radiation on the quantity and quality of organic material, and diel changes in wind intensity primarily forcing air-sea CO2 exchange, underline the value and the need of multidisciplinary campaigns for integrating SML complexity into the context of air-sea interactiones_ES
dc.language.isoen_USes_ES
dc.sourceBulletin of the American Meteorological Society, pp.1-51es_ES
dc.subjectWind-drivenes_ES
dc.subjectTurbulencees_ES
dc.subjectSolar radiationes_ES
dc.subjectSea-surfacees_ES
dc.titleThe MILAN campaign: Studying diel light effects on the air-sea interfacees_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.typeinfo:eu-repo/semantics/acceptedVersiones_ES
dc.date.updated2019-11-20T21:56:34Z
dc.identifier.doi10.1175/BAMS-D-17-0329.1
dc.description.procedenceUCR::Vicerrectoría de Investigación::Unidades de Investigación::Ciencias Básicas::Centro de Investigaciones Geofísicas (CIGEFI)es_ES
dc.description.procedenceUCR::Vicerrectoría de Docencia::Ciencias Básicas::Facultad de Ciencias::Escuela de Físicaes_ES


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