Show simple item record

dc.contributor.advisorWard, Brian
dc.contributor.authorEsters, Leonie Tabea
dc.date.accessioned2018-04-09T15:02:23Z
dc.date.available2018-04-09T15:02:23Z
dc.date.issued2018-04-09
dc.identifier.urihttp://hdl.handle.net/10379/7262
dc.description.abstractTurbulence within the ocean surface boundary layer (OSBL) is an important quantity for many processes as it mixes the ocean and transports various ocean quantities such as pollutants, heat, and dissolved gases. However, direct observations of the dissipation rate of turbulent kinetic energy \epsilon under open ocean conditions are limited. Consequently, our understanding on how to model turbulence and its related processes is constrained. Open ocean measurements from the Air-Sea Interaction Profiler (ASIP) from five cruises are combined with ship-based meteorological information, direct measurements of air-sea gas fluxes, and wave data from dedicated runs of the ECWAM wave model. This comprehensive data set allowed for an evaluation of commonly applied approaches to scale profiles of \epsilon, as well as to formulate a scaling relationship. During daytime conditions a relationship based on the friction velocity and wave age describes the observations best. During conditions when convection dominates over wind and wave-induced turbulence the scaling considers buoyancy forcing as additional source for turbulence. This data was also used to quantify the so-called small-eddy model under open-ocean conditions. This theoretical model relates air-sea gas transfer directly to turbulence, rather than often used empirical wind speed-based parameterisations. It can be shown that the agreement between the model and observations can be improved when using a variable Schmidt number exponent in the model, rather than a constant value of 1/2. Further analysis of a single deployment of ASIP in the Labrador Sea presents a unique situation where a stably stratified diurnally warmed OSBL is accompanied by a mixing event, which is most plausibly explained by a breaking internal wave. These results manifest the importance of observations in the upper ocean for understanding processes for oceanatmosphere exchange.en_IE
dc.publisherNUI Galway
dc.subjectair-sea gas exchangeen_IE
dc.subjectocean turbulenceen_IE
dc.subjectupper oceanen_IE
dc.subjectocean surface boundary layeren_IE
dc.subjectdiurnal warming eventen_IE
dc.subjectinternal wave breakingen_IE
dc.subjectPhysicsen_IE
dc.subjectScienceen_IE
dc.titleObservational based evaluation of air-sea gas fluxes and turbulence in the surface ocean boundary layeren_IE
dc.typeThesisen
dc.contributor.funderCollege of Science, National University of Ireland, Galwayen_IE
dc.local.noteOpen-ocean measurements of turbulence within the surface layer of the ocean from various research cruises were used together with meteorological and wave information were used to parameterise this turbulence and to evaluate their impact on air-sea gas exchange and diurnal warming.en_IE
dc.local.finalYesen_IE
nui.item.downloads148


Files in this item

Attribution-NonCommercial-NoDerivs 3.0 Ireland
This item is available under the Attribution-NonCommercial-NoDerivs 3.0 Ireland. No item may be reproduced for commercial purposes. Please refer to the publisher's URL where this is made available, or to notes contained in the item itself. Other terms may apply.

The following license files are associated with this item:

Thumbnail

This item appears in the following Collection(s)

Show simple item record