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dc.contributor.authorLópez Lozano, Ismael
dc.contributor.authorSánchez Hernández, Guadalupe
dc.contributor.authorGuerrero Rascado, Juan Luis 
dc.contributor.authorAlados-Arboledas, Inmaculada
dc.contributor.authorFoyo Moreno, Inmaculada 
dc.date.accessioned2022-02-22T08:13:48Z
dc.date.available2022-02-22T08:13:48Z
dc.date.issued2022-01-03
dc.identifier.urihttp://hdl.handle.net/10481/72936
dc.description.abstractThis study addresses the analysis of the cloud effects on photosynthetically active radiation (PAR, 400–700 nm) for global (PARGlobal) and its diffuse component (PARDiffuse). To this aim, a 11-year database of measured PARGlobal and modeled PARDifuse recorded in a Mediterranean site was analyzed, for both clear-sky and all-sky scenarios. PARGlobal mean values for the entire period were estimated in (200 ± 50) Wm-2 and (240 ± 50) Wm-2 for all- and clear-sky scenarios, respectively, while the values obtained for PARDiffuse were (59 ± 6) Wm-2 for all-skies and (51 ± 5) Wm-2 for clear-skies. PARGlobal monthly averages show the typical annual pattern driven by the annual course of solar position and PARDiffuse presents a similar but less marked pattern. The observed seasonal behavior was explained in terms of cloud cover, cloud frequency, liquid and ice content for allsky scenarios. Higher variability during spring was detected due to the more complex cloud features in this season. Cloud Radiative Effect (CRE) showed negative values associated with a decrease in PARGlobal (- 36 ± 14) Wm-2 and positive values corresponding to an increase in PARDiffuse (+7 ± 5) Wm-2 . A clear seasonal pattern was found for CREGlobal and CREDiffuse with higher values in spring and autumn, and lower values in summer and winter. Additionally, the PAR-to-Total ratio and diffuse fraction (kPAR) values were evaluated under different sky conditions. Monthly mean values of the PAR-to-Total ratio showed steady values around 0.44 and any dependence on clearness index (kt) nor total cloud cover (TCC) was found. However, kPAR seemed to increase with TCC, taking averages values of 0.45 for all-sky and 0.28 for clear-sky scenarios. For all-sky conditions a clear seasonal pattern was observed with higher values in colder months. A secondary maximum value for kPAR was found in summer for clear-sky scenarios, revealing the important effect of the Saharan dust intrusions in the Mediterranean region. Finally, a well-defined logistic relationship was found between kPAR and kt, leading to estimate kPAR from total solar irradiance measurements.es_ES
dc.description.sponsorshipSpanish Ministry of Economy and Competitiveness through projects CGL2016-81092-R, CGL2017-83538- C3-1-R, CGL2017-90884-REDT, PID2020-120015RB-I00 and PID2020-117825GB-C21es_ES
dc.description.sponsorshipAndalusia Regional Government, University of Granada and FEDER funds through projects B-RNM-496-UGR18, P18-RT-3820, A-RNM-430-UGR20 and B-RNM-524-UGR20es_ES
dc.description.sponsorshipEuropean Union’s Horizon 2020 research and innovation program through project ACTRIS-2 (grant agreement No 654109) and ACTRIS-IMP (grant agreement No 871115).es_ES
dc.language.isoenges_ES
dc.publisherElsevieres_ES
dc.subjectGlobal photosynthetically active radiationes_ES
dc.subjectDiffuse photosynthetically active radiationes_ES
dc.subjectCloud radiative effectes_ES
dc.subjectDiffuse fractiones_ES
dc.subjectPAR-to-Total ratioes_ES
dc.titleAnalysis of cloud effects on long-term global and diffuse photosynthetically active radiation at a Mediterranean sitees_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.relation.projectIDinfo:eu-repo/grantAgreement/EC/H2020/ACTRIS-2 654109es_ES
dc.relation.projectIDinfo:eu-repo/grantAgreement/EC/H2020/ACTRIS-IMP 871115es_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES
dc.identifier.doihttps://doi.org/10.1016/j.atmosres.2021.106010
dc.type.hasVersioninfo:eu-repo/semantics/submittedVersiones_ES


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