dc.creatorPerez, Claudio Fabian
dc.creatorBianchi, Maria Martha
dc.creatorGassmann, María Isabel
dc.creatorTonti, Natalia Edith
dc.creatorPisso, Ignacio
dc.date.accessioned2019-12-17T15:15:24Z
dc.date.accessioned2022-10-14T21:34:45Z
dc.date.available2019-12-17T15:15:24Z
dc.date.available2022-10-14T21:34:45Z
dc.date.created2019-12-17T15:15:24Z
dc.date.issued2018-11
dc.identifierPerez, Claudio Fabian; Bianchi, Maria Martha; Gassmann, María Isabel; Tonti, Natalia Edith; Pisso, Ignacio; A case study of anisotropic airborne pollen transport in Northern Patagonia using a Lagrangian particle dispersion model; Elsevier Science; Review of Palaeobotany and Palynology; 258; 11-2018; 215-222
dc.identifier0034-6667
dc.identifierhttp://hdl.handle.net/11336/92374
dc.identifierCONICET Digital
dc.identifierCONICET
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4309213
dc.description.abstractAccumulated pollen sequences are used to infer temporal changes in vegetation composition. Pollen transport and dispersal by winds introduce large biases in the interpretation of pollen records. In order to calibrate the models used to infer past species distributions, human activities or climate, contemporary time series of pollen records are assessed and modelled. The Gaussian plume model assumes that pollen transport takes place in a neutral atmosphere and pollen contribution is even from all directions (isotropy). In this study, we analyse these assumptions with airborne pollen measurements of Weinmannia trichosperma, a forest tree which grows mainly on the western slopes of the Andes, along with other characteristic species of the steppe which develops in eastern Patagonia. Instead of the Gaussian plume mixing model that is usually employed in the theory of pollen analysis, we apply a full 3D Lagrangian dispersion model, which allows calculation of potential source distributions (footprint) from modelled backward trajectories of airborne pollen observations. Results show that neutral atmospheric conditions are properly assumed for the region. The footprint calculated from the modelled trajectories of a five-year record is consistent with the location of pollen sources but the footprint shape showed that pollen contribution is uneven due to the influence of transient weather systems.
dc.languageeng
dc.publisherElsevier Science
dc.relationinfo:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0034666718301568
dc.relationinfo:eu-repo/semantics/altIdentifier/doi/http://dx.doi.org/10.1016/j.revpalbo.2018.08.007
dc.rightshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.rightsinfo:eu-repo/semantics/restrictedAccess
dc.subjectDATA TREATMENT
dc.subjectLAGRANGIAN MODEL
dc.subjectNORTHERN PATAGONIA
dc.subjectPOLLEN TRANSPORT
dc.subjectPRESENT
dc.subjectQUANTITATIVE RECONSTRUCTION
dc.titleA case study of anisotropic airborne pollen transport in Northern Patagonia using a Lagrangian particle dispersion model
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:ar-repo/semantics/artículo
dc.typeinfo:eu-repo/semantics/publishedVersion


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