{"id":107,"date":"2018-02-09T18:22:52","date_gmt":"2018-02-09T17:22:52","guid":{"rendered":"http:\/\/wp.unil.ch\/alpenv\/?page_id=107"},"modified":"2020-09-14T14:39:39","modified_gmt":"2020-09-14T12:39:39","slug":"our-projects","status":"publish","type":"page","link":"https:\/\/wp.unil.ch\/alpenv\/home\/our-projects\/","title":{"rendered":"Our Projects"},"content":{"rendered":"

Biogeomorphic feedbacks between microbes, vegetation and the physical environment following rapid glacier recession<\/a><\/strong><\/p>\n

Critical Physical Geography<\/strong><\/a><\/p>\n

Distributed measurement of bedload sediment flux in mountain catchments<\/a><\/strong><\/p>\n

Geometry and dynamics of subglacial channels<\/strong><\/a><\/p>\n

Glacier recession, glacial sediment export and the morphodynamics of proglacial forefields<\/strong><\/a><\/p>\n

Hydraulics, sediment transport and mixing at low momentum ratio junctions in Alpine drainage basins<\/strong><\/a><\/p>\n

Hydrological, geomorphological and ecosystem impacts of Alpine water intakes<\/strong><\/a><\/p>\n

Integrating lake with stream ecosystems to complete the freshwater continuum<\/strong><\/a><\/p>\n

Investigating the link between sand sediment transport and river morphodynamics<\/strong><\/a><\/p>\n

Sediment fate in a changing watershed during the Anthropocene (SEDFATE)<\/strong><\/a><\/p>\n

Stochastic downscaling and data fusion for generating synthetic high-resolution DEMs of mountain regions<\/strong><\/a><\/p>\n

Systematic error mitigation for UAV photogrammetry and application of the morphological method to gully erosion estimation<\/strong><\/a><\/p>\n

3D numerical modelling of sediment-laden river flows, morphological evolution and instream ecology<\/a><\/strong><\/p>\n

Water resource impacts of Afghan glacier recession<\/a><\/strong><\/p>\n","protected":false},"excerpt":{"rendered":"

Biogeomorphic feedbacks between microbes, vegetation and the physical environment following rapid glacier recession Critical Physical Geography Distributed measurement of bedload sediment flux in mountain catchments Geometry and dynamics of subglacial channels Glacier recession, glacial sediment export and the morphodynamics of<\/p>\n","protected":false},"author":1001734,"featured_media":0,"parent":6,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_seopress_robots_primary_cat":"","_seopress_titles_title":"","_seopress_titles_desc":"","_seopress_robots_index":"","footnotes":""},"class_list":["post-107","page","type-page","status-publish"],"_links":{"self":[{"href":"https:\/\/wp.unil.ch\/alpenv\/wp-json\/wp\/v2\/pages\/107","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/wp.unil.ch\/alpenv\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/wp.unil.ch\/alpenv\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/wp.unil.ch\/alpenv\/wp-json\/wp\/v2\/users\/1001734"}],"replies":[{"embeddable":true,"href":"https:\/\/wp.unil.ch\/alpenv\/wp-json\/wp\/v2\/comments?post=107"}],"version-history":[{"count":0,"href":"https:\/\/wp.unil.ch\/alpenv\/wp-json\/wp\/v2\/pages\/107\/revisions"}],"up":[{"embeddable":true,"href":"https:\/\/wp.unil.ch\/alpenv\/wp-json\/wp\/v2\/pages\/6"}],"wp:attachment":[{"href":"https:\/\/wp.unil.ch\/alpenv\/wp-json\/wp\/v2\/media?parent=107"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}