\n
| Name<\/th> | Description<\/th> | Funding Framework<\/th> | Period<\/th>\n<\/tr>\n<\/thead>\n | ||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| IKY Fellowship<\/td> | Development of a technological application to optimize the design of coastal infrastructure and engineering protection solutions through a risk assessment of the effects of climate change<\/td> | IKY Fellowships of Excellence for Postdoctoral Studies<\/td> | 2015-16<\/td>\n<\/tr>\n | ||||||||||||
| IKY Fellowship<\/td> | A simulation-optimization model for assessing the best practices for the protection of surface water and groundwater in the coastal zone \u201dshow_more\u201d<\/p> The 3D integrated surface water-groundwater model IRENE (Spanoudaki et al., 2009; Spanoudaki, 2010) has been modi\ufb01ed in order to simulate surface water-groundwater \ufb02ow and salinity interactions in the coastal zone. IRENE, in its original form, couples the 3D shallow water equations to the equations describing 3D saturated groundwater \ufb02ow of constant density. A semi-implicit \ufb01nite difference scheme is used to solve the surface water \ufb02ow equations, while a fully implicit \ufb01nite difference scheme is used for the groundwater equations. Pollution interactions are simulated by coupling the advection-diffusion equation describing the fate and transport of contaminants introduced in a 3D turbulent \ufb02ow \ufb01eld to the partial differential equation describing the fate and transport of contaminants in 3D transient groundwater \ufb02ow systems. The model has been further developed to include the effects of density variations on surface water and groundwater \ufb02ow, while the already built-in solute transport capabilities are used to simulate salinity interactions. The re\ufb01ned model is based on the \ufb01nite volume method using a cell-centred structured grid, providing thus \ufb02exibility and accuracy in simulating irregular boundary geometries Publication (PDF): A simulation-optimization model for effective water resources management in the coastal zone. Available from: https:\/\/www.researchgate.net\/publication\/273128146_A_simulation-optimization_model_for_effective_water_resources_management_in_the_coastal_zone [accessed Apr 5, 2017]. \u201dless\u201d<\/p><\/div><\/div><\/td> IKY Fellowships of Excellence for Postdoctoral Studies<\/td> | 2013-2015<\/td>\n<\/tr>\n | G&G Research<\/td> | 3-D numerical modelling of surface water-groundwater flow and salinity interactions in the coastal zone. | \u201dshow_more\u201d<\/p> The 3D integrated surface water-groundwater model IRENE (Spanoudaki et al., 2009; Spanoudaki, 2010) has been modified in order to simulate surface water-groundwater flow and salinity interactions in the coastal zone. IRENE, in its original form, couples the 3D, non-steady state Navier-Stokes equations, after Reynolds averaging and with the assumption of hydrostatic pressure distribution, to the equations describing 3D saturated groundwater flow of constant density. A semi-implicit finite difference scheme is used to solve the surface water flow equations, while a fully implicit finite difference scheme is used for the groundwater equations. Pollution interactions are simulated by coupling the advection-diffusion equation describing the fate and transport of contaminants introduced in a 3D turbulent flow field to the partial differential equation describing the fate and transport of contaminants in 3D transient groundwater flow systems. The model has been further developed to include the effects of density variations on surface water and groundwater flow, while the already built-in solute transport capabilities are used to simulate salinity interactions. Initial results show that IRENE can accurately predict surface water-groundwater flow and salinity interactions in coastal areas. Important research issues that can be investigated using IRENE include: (a) sea level rise and tidal effects on aquifer salinisation and the configuration of the saltwater wedge, (b) the effects of surface water-groundwater interaction on salinity increase of coastal wetlands and (c) the estimation of the location and magnitude of groundwater discharge to coasts \u201dless\u201d<\/p><\/div><\/div><\/td> Computers & Geosciences Research Scholarship Award for 2013<\/td> | 2013 - 2014<\/td>\n<\/tr>\n | HERAKLITOS \u0399\u0399<\/td> | Study of the influence of bioclimatic conditions and particulate matter air pollution to public health in Crete Island, (PI Assoc. Prof. P. Nastos, Department of Geology and Geoenvironment, National \u201cKapodistrias\u201d University of Athens), HERAKLITOS \u0399\u0399 program, Ministry of Education-Lifelong learning & Religious affairs, member of the 3member advisory committee of the PhD dissertation.<\/td> | Ministry of Education<\/td> | 2008-2011<\/td>\n<\/tr>\n | HERAKLITOS \u0399\u0399<\/td> | 17.\tMathematical and numerical modeling of the generation, and propagation of waves off shore and near shore, (PI Prof. C. Synolakis, Environmental Engineering Department Technical University of Crete), HERAKLITOS \u0399\u0399 program, Ministry of Education-Lifelong learning & Religious affairs, member of the 3member advisory committee of the PhD dissertation<\/td> | Ministry of Education<\/td> | 2008-2011<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<\/p>","protected":false},"excerpt":{"rendered":"","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-1231","page","type-page","status-publish","hentry"],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/crl.iacm.forth.gr\/en\/wp-json\/wp\/v2\/pages\/1231","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/crl.iacm.forth.gr\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/crl.iacm.forth.gr\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/crl.iacm.forth.gr\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/crl.iacm.forth.gr\/en\/wp-json\/wp\/v2\/comments?post=1231"}],"version-history":[{"count":4,"href":"https:\/\/crl.iacm.forth.gr\/en\/wp-json\/wp\/v2\/pages\/1231\/revisions"}],"predecessor-version":[{"id":1329,"href":"https:\/\/crl.iacm.forth.gr\/en\/wp-json\/wp\/v2\/pages\/1231\/revisions\/1329"}],"wp:attachment":[{"href":"https:\/\/crl.iacm.forth.gr\/en\/wp-json\/wp\/v2\/media?parent=1231"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}} | |