{"id":41,"date":"2024-04-15T10:35:27","date_gmt":"2024-04-15T10:35:27","guid":{"rendered":"https:\/\/www.atm.helsinki.fi\/icupe_wp\/?page_id=41"},"modified":"2024-04-23T12:19:46","modified_gmt":"2024-04-23T12:19:46","slug":"teasers-for-icupe-datasets","status":"publish","type":"page","link":"https:\/\/www.atm.helsinki.fi\/icupe\/?page_id=41","title":{"rendered":"Teasers for iCUPE datasets"},"content":{"rendered":"\n\n\n\n
\"ERAPLANET\"<\/a><\/td>\n\"UHEL\"<\/a><\/td>\n\"CNR\"<\/a><\/td>\n\"AarhusUniversity\"<\/a><\/td>\n\"AWI\"<\/a><\/td>\n\"CNRS\"<\/a><\/td>\n\"EULS\"<\/a><\/td>\n\"FMI\"<\/a><\/td>\n\"GFZ\"<\/a><\/td>\n\"HZG\"<\/a><\/td>\n\"NCSR\"<\/a><\/td>\n\"PSI\"<\/a><\/td>\n\"TROPOS\"<\/a><\/td>\n\"SU\"<\/a><\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n\n\n\n

Fractional snow cover area in selected sites of Svalbard islands, Norway (D3.2.2 – teaser<\/a>)<\/p>\n\n\n\n

Proxies for mixing layer height, condensation sink and gross primary production (D4.1.1 – teaser<\/a>)<\/p>\n\n\n\n

Dataset for ground-validation of precipitation measurements in high-latitudes and Arctic region, (D4.2.1 – teaser<\/a>)<\/p>\n\n\n\n

Multi-year dataset on mercury measurements at the Amderma station, Russian Arctic (teaser<\/a>)<\/p>\n\n\n\n

Elemental and organic carbon over the northwestern coast of the Kandalaksha Bay of the White Sea (teaser<\/a>)<\/p>\n\n\n\n

DS on atmospheric composition at Fonovaya Observatory, West Siberia (teaser<\/a>)<\/p>\n\n\n\n

DS on micro-climatic features and Urban Heat Island Intensity in cities of Arctic region (teaser<\/a>)<\/p>\n\n\n\n

Arctic atmospheric Hg speciation and isotope observations (D2.2.1 & 2.2.3 – teaser<\/a>)<\/p>\n\n\n\n

Time series of lake size changes in Northeast Greenland (D3.3.2 – teaser<\/a>)<\/p>\n\n\n\n

Concentration of organic contaminants, mercury and other heavy metals in annual snow and shallow core records (D2.1.1 & 2.1.2 – teaser<\/a>)<\/p>\n\n\n\n

Source apportionment of organic aerosols in the Arctic including the source regions (D1.4.2 – teaser<\/a>)<\/p>\n\n\n\n

Occurrence, transport and exchange fluxes of emerging organic contaminants in the Arctic (D2.4.1 – teaser<\/a>)<\/p>\n\n\n\n

Investigating the small-scale vertical and horizontal variability of the atmospheric boundary layer aerosol using unmanned aerial systems (D1.3.2 – teaser<\/a>) <\/p>\n\n\n\n

Absorption Coefficient \/ Equivalent Black Carbon standardized dataset for long term impacts in the Arctic (D1.2.1 – teaser<\/a>)<\/p>\n\n\n\n

Continuous vertical observation of aerosol and cloud properties during the Polarstern cruises PS 106.1 and PS106.2 using a CLOUDNET station (D1.3.2-n2 – teaser<\/a>)<\/p>\n\n\n\n

Dataset and code on classification of artificial light sources (D3.2.2-a – teaser<\/a>)<\/p>\n\n\n\n

Visible Near Infrared (VNIR) airborne and simulated EnMAP satellite hyperspectral imagery of Toolik Lake, Alaska (D3.2.2-b – teaser<\/a>)<\/p>\n\n\n\n

Dataset of validated aerosol vertical profiles from ground-based and satellite observations above selected sites in Finland (D4.3.1-a – teaser<\/a>)<\/p>\n\n\n\n

Aerosol physical and optical characteristics including equivalent black carbon at Ny-Alesund, Svalbard (D1.1.2 – teaser<\/a>)<\/p>\n\n\n\n

Snow spectral reflectance measurements at Ny-Alesund, Svalbard (D1.1.3 – teaser<\/a>)<\/p>\n\n\n\n

Vertical profiles of equivalent black carbon in the Arctic boundary layer at Ny-\u00c5lesund, Svalbard (D1.3.2b – teaser<\/a>)<\/p>\n","protected":false},"excerpt":{"rendered":"

Fractional snow cover area in selected sites of Svalbard islands, Norway (D3.2.2 – teaser) Proxies for mixing layer height, condensation […]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"default","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"default","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""}},"footnotes":""},"class_list":["post-41","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/www.atm.helsinki.fi\/icupe\/index.php?rest_route=\/wp\/v2\/pages\/41","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.atm.helsinki.fi\/icupe\/index.php?rest_route=\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.atm.helsinki.fi\/icupe\/index.php?rest_route=\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.atm.helsinki.fi\/icupe\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.atm.helsinki.fi\/icupe\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=41"}],"version-history":[{"count":2,"href":"https:\/\/www.atm.helsinki.fi\/icupe\/index.php?rest_route=\/wp\/v2\/pages\/41\/revisions"}],"predecessor-version":[{"id":84,"href":"https:\/\/www.atm.helsinki.fi\/icupe\/index.php?rest_route=\/wp\/v2\/pages\/41\/revisions\/84"}],"wp:attachment":[{"href":"https:\/\/www.atm.helsinki.fi\/icupe\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=41"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}