https://w3id.org/np/RAP2P7SYOHe23ItJJmcFm0BASk2pcIZLfkpByaqz0eBDo/Head https://w3id.org/np/RAP2P7SYOHe23ItJJmcFm0BASk2pcIZLfkpByaqz0eBDo http://www.nanopub.org/nschema#hasAssertion https://w3id.org/np/RAP2P7SYOHe23ItJJmcFm0BASk2pcIZLfkpByaqz0eBDo/assertion https://w3id.org/np/RAP2P7SYOHe23ItJJmcFm0BASk2pcIZLfkpByaqz0eBDo http://www.nanopub.org/nschema#hasProvenance https://w3id.org/np/RAP2P7SYOHe23ItJJmcFm0BASk2pcIZLfkpByaqz0eBDo/provenance https://w3id.org/np/RAP2P7SYOHe23ItJJmcFm0BASk2pcIZLfkpByaqz0eBDo http://www.nanopub.org/nschema#hasPublicationInfo https://w3id.org/np/RAP2P7SYOHe23ItJJmcFm0BASk2pcIZLfkpByaqz0eBDo/pubinfo https://w3id.org/np/RAP2P7SYOHe23ItJJmcFm0BASk2pcIZLfkpByaqz0eBDo http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://www.nanopub.org/nschema#Nanopublication https://w3id.org/np/RAP2P7SYOHe23ItJJmcFm0BASk2pcIZLfkpByaqz0eBDo/assertion http://eurovoc.europa.eu/3949 http://schema.org/description http://eurovoc.europa.eu/3949 http://schema.org/name Applied sciences http://eurovoc.europa.eu/3949 http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://schema.org/DefinedTerm http://w3id.org/ro-id/rohub/model#funder/77e874cf-1d8a-4a19-8aa2-abef43e07850 http://purl.org/ontology/bibo/doi 10.13039/501100007601 http://w3id.org/ro-id/rohub/model#funder/77e874cf-1d8a-4a19-8aa2-abef43e07850 http://schema.org/name Horizon 2020 http://w3id.org/ro-id/rohub/model#funder/77e874cf-1d8a-4a19-8aa2-abef43e07850 http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://schema.org/Organization http://w3id.org/ro-id/rohub/model#funder/f5d47dbc-4fcb-451c-8d92-8f50424e9d20 http://purl.org/ontology/bibo/doi 10.13039/100010662 http://w3id.org/ro-id/rohub/model#funder/f5d47dbc-4fcb-451c-8d92-8f50424e9d20 http://schema.org/name H2020 Excellent Science http://w3id.org/ro-id/rohub/model#funder/f5d47dbc-4fcb-451c-8d92-8f50424e9d20 http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://schema.org/Organization https://besjournals-onlinelibrary-wiley-com.ezproxy.uio.no/doi/10.1111/j.1365-2745.2011.01859.x http://schema.org/author https://orcid.org/0000-0002-8763-1643 https://besjournals-onlinelibrary-wiley-com.ezproxy.uio.no/doi/10.1111/j.1365-2745.2011.01859.x http://schema.org/contentUrl https://besjournals-onlinelibrary-wiley-com.ezproxy.uio.no/doi/10.1111/j.1365-2745.2011.01859.x https://besjournals-onlinelibrary-wiley-com.ezproxy.uio.no/doi/10.1111/j.1365-2745.2011.01859.x http://schema.org/creator https://orcid.org/0000-0002-8763-1643 https://besjournals-onlinelibrary-wiley-com.ezproxy.uio.no/doi/10.1111/j.1365-2745.2011.01859.x http://schema.org/dateCreated 2024-01-09 13:23:52.056842+00:00 https://besjournals-onlinelibrary-wiley-com.ezproxy.uio.no/doi/10.1111/j.1365-2745.2011.01859.x http://schema.org/dateModified 2024-01-09 13:23:53.583909+00:00 https://besjournals-onlinelibrary-wiley-com.ezproxy.uio.no/doi/10.1111/j.1365-2745.2011.01859.x http://schema.org/description Summary: Climate change in northern high latitudes is predicted to be greater in winter rather than summer, yet little is known about the effects of winter climate change on northern ecosystems. Among the unknowns are the effects of an increasing frequency of acute, short-lasting winter warming events. Such events can damage higher plants exposed to warm, then returning cold, temperatures after snow melt, and it is not known how bryophytes and lichens, which are of considerable ecological importance in high-latitude ecosystems, are affected by such warming events. However, even physiological adaptations of these cryptogams to winter environments in general are poorly understood. Here we describe findings from a novel field experiment that uses heating from infrared lamps and soil warming cables to simulate acute mid-winter warming events in a sub-Arctic heath. In particular, we report the growing season responses of the dominant lichen, Peltigera aphthosa, and bryophyte, Hylocomium splendens, to warming events in three consecutive winters. While summertime photosynthetic performance of P. aphthosa was unaffected by the winter warming treatments, H. splendens showed significant reductions in net photosynthetic rates and growth rates (of up to 48% and 52%, respectively). Negative effects were evident already during the summer following the first winter warming event. While the lichen develops without going through critical phenological stages during which vulnerable organs are produced, the moss has a seasonal rhythm, which includes initiation of growth of young, freeze-susceptible shoot apices in the early growing season; these might be damaged by breaking of dormancy during warm winter events. Synthesis. Different sensitivities of the bryophyte and lichen species were unexpected, and illustrate that very little is known about the winter ecology of bryophytes and lichens from cold biomes in general. In sharp contrast to summer warming experiments that show increased vascular plant biomass and reduced lichen biomass, these results demonstrate that acute climate events in mid-winter may be readily tolerated by lichens, in contrast to previously observed sensitivity of co-occurring dwarf shrubs, suggesting winter climate change may compensate for (or even reverse) predicted lichen declines resulting from summer warming. https://besjournals-onlinelibrary-wiley-com.ezproxy.uio.no/doi/10.1111/j.1365-2745.2011.01859.x http://schema.org/keywords Winter warming https://besjournals-onlinelibrary-wiley-com.ezproxy.uio.no/doi/10.1111/j.1365-2745.2011.01859.x http://schema.org/license https://choosealicense.com/no-permission/ https://besjournals-onlinelibrary-wiley-com.ezproxy.uio.no/doi/10.1111/j.1365-2745.2011.01859.x http://schema.org/name Contrasting sensitivity to extreme winter warming events of dominant sub‐Arctic heathland bryophyte and lichen species https://besjournals-onlinelibrary-wiley-com.ezproxy.uio.no/doi/10.1111/j.1365-2745.2011.01859.x http://schema.org/sdDatePublished 2024-01-09 13:23:52.056842+00:00 https://besjournals-onlinelibrary-wiley-com.ezproxy.uio.no/doi/10.1111/j.1365-2745.2011.01859.x http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://purl.org/wf4ever/wf4ever#Resource https://besjournals-onlinelibrary-wiley-com.ezproxy.uio.no/doi/10.1111/j.1365-2745.2011.01859.x http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://schema.org/Article https://besjournals-onlinelibrary-wiley-com.ezproxy.uio.no/doi/10.1111/j.1365-2745.2011.01859.x http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://schema.org/MediaObject https://doi.org/10.1016/j.jhydrol.2022.128593 http://schema.org/author https://orcid.org/0000-0002-8763-1643 https://doi.org/10.1016/j.jhydrol.2022.128593 http://schema.org/contentUrl https://doi.org/10.1016/j.jhydrol.2022.128593 https://doi.org/10.1016/j.jhydrol.2022.128593 http://schema.org/creator https://orcid.org/0000-0002-8763-1643 https://doi.org/10.1016/j.jhydrol.2022.128593 http://schema.org/dateCreated 2022-11-17 12:42:58.014321+00:00 https://doi.org/10.1016/j.jhydrol.2022.128593 http://schema.org/dateModified 2022-11-17 12:42:59.601045+00:00 https://doi.org/10.1016/j.jhydrol.2022.128593 http://schema.org/description Rain-on-snow (ROS) events can greatly affect the snow process and cause severe snowmelt-related hazards. It is important to monitor the spatiotemporal distribution of ROS events over the ungauged High Mountain Asia (HMA). This study investigated the spatiotemporal variability of ROS events over the HMA and its potential influencing factors from 1981 to 2020 based on stand-alone Noah-MP land surface model simulations forced by hourly HARv2 reanalysis dataset. The results demonstrated that ROS activity occurred more frequently in the higher-elevation (2500–4000 m and 5500–6000 m a.s.l) regions of the Tianshan Mountains, Pamir, eastern Hindu Kush, Himalayas, and the western Hengduan Shan, with an annual maximum ROS frequency exceeding 15 days and a maximum intensity reaching 40 mm concentrated in spring and summer. ROS frequency experienced a significant decrease in the high-elevation (3000–4500 m a.s.l) regions of the eastern Hindu Kush, West Himalaya, and western Hengduan Shan with a rate exceeding −1.5 days/decade. The decrease in ROS frequency could be explained by a shifting of precipitation type from snowfall to rain driven by dramatic warming and resulting in a decline in snowfall and shortened snow cover persistence, particularly in spring and summer. On the contrary, significantly increasing trend mainly prevailed in the high-elevation (5000–6000 m a.s.l) regions of Transhimalaya and East Himalaya, exceeding 0.9 days/decade. https://doi.org/10.1016/j.jhydrol.2022.128593 http://schema.org/license https://choosealicense.com/no-permission/ https://doi.org/10.1016/j.jhydrol.2022.128593 http://schema.org/name Trends and spatial variations of rain-on-snow events over the high Mountain Asia https://doi.org/10.1016/j.jhydrol.2022.128593 http://schema.org/sdDatePublished 2022-11-17 12:42:58.014321+00:00 https://doi.org/10.1016/j.jhydrol.2022.128593 http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://purl.org/wf4ever/roterms#Paper https://doi.org/10.1016/j.jhydrol.2022.128593 http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://purl.org/wf4ever/wf4ever#Resource https://doi.org/10.1016/j.jhydrol.2022.128593 http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://schema.org/MediaObject https://doi.org/10.2307/1550592 http://schema.org/author https://orcid.org/0000-0002-8763-1643 https://doi.org/10.2307/1550592 http://schema.org/contentUrl https://doi.org/10.2307/1550592 https://doi.org/10.2307/1550592 http://schema.org/creator https://orcid.org/0000-0002-8763-1643 https://doi.org/10.2307/1550592 http://schema.org/dateCreated 2023-04-05 15:02:43.479985+00:00 https://doi.org/10.2307/1550592 http://schema.org/dateModified 2023-04-05 15:02:46.070674+00:00 https://doi.org/10.2307/1550592 http://schema.org/description ABSTRACT The origin of lichen-free areas in the High Arctic has been attributed to lichen-kill under permanent snowfields developed 300 yr ago during the Little Ice Age. There are inconsistencies in this hypothesis, particularly in regard to the manner of lichen-kill, the mechanism of dead lichen removal once the previously ice-covered ground is exposed again, the period when the lichen-kill occured, and the form of lichen trimlines. An alternative hypothesis is suggested whereby lichen-free areas occur where seasonal snowfields persist for a much greater part of the summer than elsewhere. As a result the lichen growth season there is very short. https://doi.org/10.2307/1550592 http://schema.org/keywords lichen-kill https://doi.org/10.2307/1550592 http://schema.org/license https://choosealicense.com/no-permission/ https://doi.org/10.2307/1550592 http://schema.org/name The Problem of Lichen-Free Zones in Arctic Canada https://doi.org/10.2307/1550592 http://schema.org/sdDatePublished 2023-04-05 15:02:43.479985+00:00 https://doi.org/10.2307/1550592 http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://purl.org/wf4ever/roterms#Paper https://doi.org/10.2307/1550592 http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://purl.org/wf4ever/wf4ever#Resource https://doi.org/10.2307/1550592 http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://schema.org/MediaObject https://doi.org/10.5194/egusphere-egu23-2579 http://schema.org/author https://orcid.org/0000-0002-1784-2920 https://doi.org/10.5194/egusphere-egu23-2579 http://schema.org/contentUrl https://doi.org/10.5194/egusphere-egu23-2579 https://doi.org/10.5194/egusphere-egu23-2579 http://schema.org/creator https://orcid.org/0000-0002-1784-2920 https://doi.org/10.5194/egusphere-egu23-2579 http://schema.org/dateCreated 2023-05-06 08:25:46.657077+00:00 https://doi.org/10.5194/egusphere-egu23-2579 http://schema.org/dateModified 2023-05-06 08:25:47.523870+00:00 https://doi.org/10.5194/egusphere-egu23-2579 http://schema.org/description Summary submitted at EGU 2023. https://doi.org/10.5194/egusphere-egu23-2579 http://schema.org/license https://choosealicense.com/no-permission/ https://doi.org/10.5194/egusphere-egu23-2579 http://schema.org/name Using FAIR and Open Science practices to better understand vegetation browning in Troms and Finnmark (Norway) https://doi.org/10.5194/egusphere-egu23-2579 http://schema.org/sdDatePublished 2023-05-06 08:25:46.657077+00:00 https://doi.org/10.5194/egusphere-egu23-2579 http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://purl.org/wf4ever/wf4ever#Resource https://doi.org/10.5194/egusphere-egu23-2579 http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://schema.org/MediaObject https://doi.org/10.5194/egusphere-egu23-2579 http://www.w3.org/1999/02/22-rdf-syntax-ns#type https://w3id.org/ro/terms/earth-science#ConferencePaper https://hess.copernicus.org/articles/23/2983/2019/hess-23-2983-2019.pdf http://schema.org/author https://orcid.org/0000-0002-8763-1643 https://hess.copernicus.org/articles/23/2983/2019/hess-23-2983-2019.pdf http://schema.org/contentUrl https://hess.copernicus.org/articles/23/2983/2019/hess-23-2983-2019.pdf https://hess.copernicus.org/articles/23/2983/2019/hess-23-2983-2019.pdf http://schema.org/creator https://orcid.org/0000-0002-8763-1643 https://hess.copernicus.org/articles/23/2983/2019/hess-23-2983-2019.pdf http://schema.org/dateCreated 2023-04-05 12:52:29.688139+00:00 https://hess.copernicus.org/articles/23/2983/2019/hess-23-2983-2019.pdf http://schema.org/dateModified 2023-04-05 12:52:36.003321+00:00 https://hess.copernicus.org/articles/23/2983/2019/hess-23-2983-2019.pdf http://schema.org/description Abstract. Rain-on-snow (ROS) events in mountainous catchments can cause enhanced snowmelt, leading to an increased risk of destructive winter floods. However, due to differences in topography and forest cover, the generation of snowpack outflow volumes and their contribution to streamflow are spatially and temporally variable during ROS events. In order to adequately predict such flood events with hydrological models, an enhanced process understanding of the contribution of rainwater and snowmelt to stream water is needed. https://hess.copernicus.org/articles/23/2983/2019/hess-23-2983-2019.pdf http://schema.org/encodingFormat application/pdf https://hess.copernicus.org/articles/23/2983/2019/hess-23-2983-2019.pdf http://schema.org/keywords rain-on-snow https://hess.copernicus.org/articles/23/2983/2019/hess-23-2983-2019.pdf http://schema.org/license https://choosealicense.com/no-permission/ https://hess.copernicus.org/articles/23/2983/2019/hess-23-2983-2019.pdf http://schema.org/name Monitoring snowpack outflow volumes and their isotopic composition to better understand streamflow generation during rain-on-snow events https://hess.copernicus.org/articles/23/2983/2019/hess-23-2983-2019.pdf http://schema.org/sdDatePublished 2023-04-05 12:52:29.688139+00:00 https://hess.copernicus.org/articles/23/2983/2019/hess-23-2983-2019.pdf http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://purl.org/wf4ever/roterms#Paper https://hess.copernicus.org/articles/23/2983/2019/hess-23-2983-2019.pdf http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://purl.org/wf4ever/wf4ever#Resource https://hess.copernicus.org/articles/23/2983/2019/hess-23-2983-2019.pdf http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://schema.org/MediaObject https://munin.uit.no/bitstream/handle/10037/28742/article.pdf?sequence=2 http://schema.org/author https://orcid.org/0000-0002-8763-1643 https://munin.uit.no/bitstream/handle/10037/28742/article.pdf?sequence=2 http://schema.org/contentUrl https://munin.uit.no/bitstream/handle/10037/28742/article.pdf?sequence=2 https://munin.uit.no/bitstream/handle/10037/28742/article.pdf?sequence=2 http://schema.org/creator https://orcid.org/0000-0002-8763-1643 https://munin.uit.no/bitstream/handle/10037/28742/article.pdf?sequence=2 http://schema.org/dateCreated 2023-04-05 15:35:11.553400+00:00 https://munin.uit.no/bitstream/handle/10037/28742/article.pdf?sequence=2 http://schema.org/dateModified 2023-04-05 15:36:09.779957+00:00 https://munin.uit.no/bitstream/handle/10037/28742/article.pdf?sequence=2 http://schema.org/description Abstract Arctic ecosystems are increasingly exposed to extreme climatic events throughout the year, which can affect species performance. Cryptogams (bryophytes and lichens) provide important ecosystem services in polar ecosystems but may be physiologically affected or killed by extreme events. Through field and laboratory manipulations, we compared physiological responses of seven dominant sub-Arctic cryptogams (three bryophytes, four lichens) to single events and factorial combinations of mid-winter heatwave (6
C for 7 days), re-freezing, snow removal and summer nitrogen addition. We aimed to identify which mosses and lichens are vulnerable to these abiotic extremes and if combinations would exacerbate physiological responses. Combinations of extremes resulted in stronger species responses but included idiosyncratic species-specific responses. Species that remained dormant during winter (March), irrespective of extremes, showed little physiological response during summer (August). However, winter physiological activity, and response to winter extremes, was not consistently associated with summer physiological impacts. Winter extremes affect cryptogam physiology, but summer responses appear mild, and lichens affect the photobiont more than the mycobiont. Accounting for Arctic cryptogam response to multiple climatic extremes in ecosystem functioning and modelling will require a better understanding of their winter eco-physiology and repair capabilities. https://munin.uit.no/bitstream/handle/10037/28742/article.pdf?sequence=2 http://schema.org/encodingFormat application/pdf https://munin.uit.no/bitstream/handle/10037/28742/article.pdf?sequence=2 http://schema.org/keywords winter heatwaves https://munin.uit.no/bitstream/handle/10037/28742/article.pdf?sequence=2 http://schema.org/license https://choosealicense.com/no-permission/ https://munin.uit.no/bitstream/handle/10037/28742/article.pdf?sequence=2 http://schema.org/name Sub-arctic mosses and lichens show idiosyncratic responses to combinations of winter heatwaves, freezing and nitrogen deposition https://munin.uit.no/bitstream/handle/10037/28742/article.pdf?sequence=2 http://schema.org/sdDatePublished 2023-04-05 15:35:11.553400+00:00 https://munin.uit.no/bitstream/handle/10037/28742/article.pdf?sequence=2 http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://purl.org/wf4ever/roterms#Paper https://munin.uit.no/bitstream/handle/10037/28742/article.pdf?sequence=2 http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://purl.org/wf4ever/wf4ever#Resource https://munin.uit.no/bitstream/handle/10037/28742/article.pdf?sequence=2 http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://schema.org/MediaObject https://onlinelibrary.wiley.com/doi/full/10.1111/gcb.14500 http://schema.org/author https://orcid.org/0000-0002-8763-1643 https://onlinelibrary.wiley.com/doi/full/10.1111/gcb.14500 http://schema.org/contentUrl https://onlinelibrary.wiley.com/doi/full/10.1111/gcb.14500 https://onlinelibrary.wiley.com/doi/full/10.1111/gcb.14500 http://schema.org/creator https://orcid.org/0000-0002-8763-1643 https://onlinelibrary.wiley.com/doi/full/10.1111/gcb.14500 http://schema.org/dateCreated 2023-05-12 06:52:53.437701+00:00 https://onlinelibrary.wiley.com/doi/full/10.1111/gcb.14500 http://schema.org/dateModified 2023-05-12 06:52:57.978371+00:00 https://onlinelibrary.wiley.com/doi/full/10.1111/gcb.14500 http://schema.org/description Abstract Extreme climatic events are among the drivers of recent declines in plant biomass and productivity observed across Arctic ecosystems, known as “Arctic browning.” These events can cause landscape-scale vegetation damage and so are likely to have major impacts on ecosystem CO2 balance. However, there is little understanding of the impacts on CO2 fluxes, especially across the growing season. Furthermore, while widespread shoot mortality is commonly observed with browning events, recent observations show that shoot stress responses are also common, and manifest as high levels of persistent anthocyanin pigmentation. Whether or how this response impacts ecosystem CO2 fluxes is not known. To address these research needs, a growing season assessment of browning impacts following frost drought and extreme winter warming (both extreme climatic events) on the key ecosystem CO2 fluxes Net Ecosystem Exchange (NEE), Gross Primary Productivity (GPP), ecosystem respiration (Reco) and soil respiration (Rsoil) was carried out in widespread sub-Arctic dwarf shrub heathland, incorporating both mortality and stress responses. Browning (mortality and stress responses combined) caused considerable site-level reductions in GPP and NEE (of up to 44%), with greatest impacts occurring at early and late season. Furthermore, impacts on CO2 fluxes associated with stress often equalled or exceeded those resulting from vegetation mortality. This demonstrates that extreme events can have major impac https://onlinelibrary.wiley.com/doi/full/10.1111/gcb.14500 http://schema.org/keywords Arctic browning https://onlinelibrary.wiley.com/doi/full/10.1111/gcb.14500 http://schema.org/keywords CO2 fluxes https://onlinelibrary.wiley.com/doi/full/10.1111/gcb.14500 http://schema.org/license https://choosealicense.com/no-permission/ https://onlinelibrary.wiley.com/doi/full/10.1111/gcb.14500 http://schema.org/name Arctic browning: Impacts of extreme climatic events on heathland ecosystem CO2 fluxes https://onlinelibrary.wiley.com/doi/full/10.1111/gcb.14500 http://schema.org/sdDatePublished 2023-05-12 06:52:53.437701+00:00 https://onlinelibrary.wiley.com/doi/full/10.1111/gcb.14500 http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://purl.org/wf4ever/roterms#Paper https://onlinelibrary.wiley.com/doi/full/10.1111/gcb.14500 http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://purl.org/wf4ever/wf4ever#Resource https://onlinelibrary.wiley.com/doi/full/10.1111/gcb.14500 http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://schema.org/MediaObject https://orcid.org/0000-0002-1784-2920 http://schema.org/affiliation Simula Research Laboratory https://orcid.org/0000-0002-1784-2920 http://schema.org/email annef@simula.no https://orcid.org/0000-0002-1784-2920 http://schema.org/name Anne Fouilloux https://orcid.org/0000-0002-1784-2920 http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://xmlns.com/foaf/0.1/Agent https://orcid.org/0000-0002-1784-2920 https://w3id.org/dingo#orcid 0000-0002-1784-2920 https://orcid.org/0000-0002-8763-1643 http://schema.org/email jeani@uio.no https://orcid.org/0000-0002-8763-1643 http://schema.org/name Jean Iaquinta https://orcid.org/0000-0002-8763-1643 http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://xmlns.com/foaf/0.1/Agent https://orcid.org/0000-0002-8763-1643 https://w3id.org/dingo#orcid 0000-0002-8763-1643 https://raw.githubusercontent.com/j34ni/Vegetation_in_Troms_and_Finnmark/main/train_mooc_tp1n.ipynb http://schema.org/author https://orcid.org/0000-0002-1784-2920 https://raw.githubusercontent.com/j34ni/Vegetation_in_Troms_and_Finnmark/main/train_mooc_tp1n.ipynb http://schema.org/contentUrl https://raw.githubusercontent.com/j34ni/Vegetation_in_Troms_and_Finnmark/main/train_mooc_tp1n.ipynb https://raw.githubusercontent.com/j34ni/Vegetation_in_Troms_and_Finnmark/main/train_mooc_tp1n.ipynb http://schema.org/creator https://orcid.org/0000-0002-1784-2920 https://raw.githubusercontent.com/j34ni/Vegetation_in_Troms_and_Finnmark/main/train_mooc_tp1n.ipynb http://schema.org/dateCreated 2023-03-26 12:00:45.352407+00:00 https://raw.githubusercontent.com/j34ni/Vegetation_in_Troms_and_Finnmark/main/train_mooc_tp1n.ipynb http://schema.org/dateModified 2023-04-12 19:21:53.527818+00:00 https://raw.githubusercontent.com/j34ni/Vegetation_in_Troms_and_Finnmark/main/train_mooc_tp1n.ipynb http://schema.org/description Jupyter Notebook for training, testing and validating machine learning method to forecast moss and lichen fractional cover mean. 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However in certain regions, especially in the Arctic, there are areas exhibiting a browning trend. 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https://w3id.org/ro/terms/earth-science#IPTC https://w3id.org/ro-id/enrichment/4561ba46-107c-43aa-8897-7e655b09a2cb https://w3id.org/ro/terms/earth-science#path Human interest/Plant https://w3id.org/ro-id/enrichment/4a6641bf-c27e-4803-a945-e6861e046ec5 http://schema.org/name browning trend https://w3id.org/ro-id/enrichment/4a6641bf-c27e-4803-a945-e6861e046ec5 http://www.w3.org/1999/02/22-rdf-syntax-ns#type https://w3id.org/ro/terms/earth-science#Phrase https://w3id.org/ro-id/enrichment/4a6641bf-c27e-4803-a945-e6861e046ec5 https://w3id.org/ro/terms/earth-science#normScore 34.63626492942454 https://w3id.org/ro-id/enrichment/4a6641bf-c27e-4803-a945-e6861e046ec5 https://w3id.org/ro/terms/earth-science#score 31.9 https://w3id.org/ro-id/enrichment/4ba86de6-05c5-45c1-8021-368608bbea91 http://schema.org/name However in certain regions, especially in the Arctic, there are areas exhibiting a browning trend. https://w3id.org/ro-id/enrichment/4ba86de6-05c5-45c1-8021-368608bbea91 http://www.w3.org/1999/02/22-rdf-syntax-ns#type https://w3id.org/ro/terms/earth-science#Sentence https://w3id.org/ro-id/enrichment/4ba86de6-05c5-45c1-8021-368608bbea91 https://w3id.org/ro/terms/earth-science#normScore 10.470085470085472 https://w3id.org/ro-id/enrichment/4ba86de6-05c5-45c1-8021-368608bbea91 https://w3id.org/ro/terms/earth-science#score 9.8 https://w3id.org/ro-id/enrichment/4c1db303-9786-4daa-98a3-eb2f4c798926 http://schema.org/name vegetation https://w3id.org/ro-id/enrichment/4c1db303-9786-4daa-98a3-eb2f4c798926 http://www.w3.org/1999/02/22-rdf-syntax-ns#type https://w3id.org/ro/terms/earth-science#Concept https://w3id.org/ro-id/enrichment/4c1db303-9786-4daa-98a3-eb2f4c798926 https://w3id.org/ro/terms/earth-science#normScore 11.088504577822992 https://w3id.org/ro-id/enrichment/4c1db303-9786-4daa-98a3-eb2f4c798926 https://w3id.org/ro/terms/earth-science#score 10.9 https://w3id.org/ro-id/enrichment/51ffa0bd-e13d-416e-aa32-0c84e971988a http://schema.org/name vegetation https://w3id.org/ro-id/enrichment/51ffa0bd-e13d-416e-aa32-0c84e971988a http://www.w3.org/1999/02/22-rdf-syntax-ns#type https://w3id.org/ro/terms/earth-science#Lemma https://w3id.org/ro-id/enrichment/51ffa0bd-e13d-416e-aa32-0c84e971988a https://w3id.org/ro/terms/earth-science#normScore 15.482954545454545 https://w3id.org/ro-id/enrichment/51ffa0bd-e13d-416e-aa32-0c84e971988a https://w3id.org/ro/terms/earth-science#score 10.9 https://w3id.org/ro-id/enrichment/5cf5d128-5270-48fa-bf3f-2f52930f7e64 http://schema.org/name browning https://w3id.org/ro-id/enrichment/5cf5d128-5270-48fa-bf3f-2f52930f7e64 http://www.w3.org/1999/02/22-rdf-syntax-ns#type https://w3id.org/ro/terms/earth-science#Lemma https://w3id.org/ro-id/enrichment/5cf5d128-5270-48fa-bf3f-2f52930f7e64 https://w3id.org/ro/terms/earth-science#normScore 9.801136363636363 https://w3id.org/ro-id/enrichment/5cf5d128-5270-48fa-bf3f-2f52930f7e64 https://w3id.org/ro/terms/earth-science#score 6.9 https://w3id.org/ro-id/enrichment/620d1bfa-e151-4320-a4e8-ab43222fb735 http://schema.org/name Arctic Zone https://w3id.org/ro-id/enrichment/620d1bfa-e151-4320-a4e8-ab43222fb735 http://www.w3.org/1999/02/22-rdf-syntax-ns#type https://w3id.org/ro/terms/earth-science#Lemma https://w3id.org/ro-id/enrichment/620d1bfa-e151-4320-a4e8-ab43222fb735 https://w3id.org/ro/terms/earth-science#normScore 9.801136363636363 https://w3id.org/ro-id/enrichment/620d1bfa-e151-4320-a4e8-ab43222fb735 https://w3id.org/ro/terms/earth-science#score 6.9 https://w3id.org/ro-id/enrichment/629e390c-9796-45d4-adf3-7f4f7e70bb92 http://schema.org/name Troms Fylke https://w3id.org/ro-id/enrichment/629e390c-9796-45d4-adf3-7f4f7e70bb92 http://www.w3.org/1999/02/22-rdf-syntax-ns#type https://w3id.org/ro/terms/earth-science#Concept https://w3id.org/ro-id/enrichment/629e390c-9796-45d4-adf3-7f4f7e70bb92 https://w3id.org/ro/terms/earth-science#normScore 15.361139369277721 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https://w3id.org/ro/terms/earth-science#normScore 47.36842105263158 https://w3id.org/ro-id/enrichment/6b53734d-4049-4ed0-901b-839d249addd6 https://w3id.org/ro/terms/earth-science#score 0.9 https://w3id.org/ro-id/enrichment/6cf9ed48-314d-44bb-9389-7840db0d8cd6 http://schema.org/name Troms Fylke https://w3id.org/ro-id/enrichment/6cf9ed48-314d-44bb-9389-7840db0d8cd6 http://www.w3.org/1999/02/22-rdf-syntax-ns#type https://w3id.org/contentdesc#Place https://w3id.org/ro-id/enrichment/6cf9ed48-314d-44bb-9389-7840db0d8cd6 https://w3id.org/ro/terms/earth-science#wikidata https://www.wikidata.org/wiki/Q50631 https://w3id.org/ro-id/enrichment/70d461e2-58a7-45c8-857c-b9d9086565b5 http://schema.org/name trend https://w3id.org/ro-id/enrichment/70d461e2-58a7-45c8-857c-b9d9086565b5 http://www.w3.org/1999/02/22-rdf-syntax-ns#type https://w3id.org/ro/terms/earth-science#Concept https://w3id.org/ro-id/enrichment/70d461e2-58a7-45c8-857c-b9d9086565b5 https://w3id.org/ro/terms/earth-science#normScore 5.0864699898270604 https://w3id.org/ro-id/enrichment/70d461e2-58a7-45c8-857c-b9d9086565b5 https://w3id.org/ro/terms/earth-science#score 5.0 https://w3id.org/ro-id/enrichment/7d0a613a-0da5-456f-9679-b4484a1cd99b http://schema.org/name Here we focus on the Troms and Finnmark counties in northern Norway to assess the extend of the phenomenon and any link with local environmental conditions. https://w3id.org/ro-id/enrichment/7d0a613a-0da5-456f-9679-b4484a1cd99b http://www.w3.org/1999/02/22-rdf-syntax-ns#type https://w3id.org/ro/terms/earth-science#Sentence https://w3id.org/ro-id/enrichment/7d0a613a-0da5-456f-9679-b4484a1cd99b https://w3id.org/ro/terms/earth-science#normScore 23.183760683760685 https://w3id.org/ro-id/enrichment/7d0a613a-0da5-456f-9679-b4484a1cd99b https://w3id.org/ro/terms/earth-science#score 21.7 https://w3id.org/ro-id/enrichment/8246be39-6a1c-438c-81b5-c9ad4579227f http://schema.org/name Norway https://w3id.org/ro-id/enrichment/8246be39-6a1c-438c-81b5-c9ad4579227f http://www.w3.org/1999/02/22-rdf-syntax-ns#type https://w3id.org/ro/terms/earth-science#Concept https://w3id.org/ro-id/enrichment/8246be39-6a1c-438c-81b5-c9ad4579227f https://w3id.org/ro/terms/earth-science#normScore 7.426246185147508 https://w3id.org/ro-id/enrichment/8246be39-6a1c-438c-81b5-c9ad4579227f https://w3id.org/ro/terms/earth-science#score 7.3 https://w3id.org/ro-id/enrichment/8b42dbec-334d-4e2b-babc-9d3aecd42347 http://schema.org/name geology https://w3id.org/ro-id/enrichment/8b42dbec-334d-4e2b-babc-9d3aecd42347 http://www.w3.org/1999/02/22-rdf-syntax-ns#type https://w3id.org/ro/terms/earth-science#FieldOfResearch https://w3id.org/ro-id/enrichment/8b42dbec-334d-4e2b-babc-9d3aecd42347 https://w3id.org/ro/terms/earth-science#normScore 100.0 https://w3id.org/ro-id/enrichment/8b42dbec-334d-4e2b-babc-9d3aecd42347 https://w3id.org/ro/terms/earth-science#score 0.7859669327735901 https://w3id.org/ro-id/enrichment/918b5844-10ad-4297-9a29-f6230b3a0068 http://schema.org/name Norway https://w3id.org/ro-id/enrichment/918b5844-10ad-4297-9a29-f6230b3a0068 http://www.w3.org/1999/02/22-rdf-syntax-ns#type https://w3id.org/ro/terms/earth-science#Lemma https://w3id.org/ro-id/enrichment/918b5844-10ad-4297-9a29-f6230b3a0068 https://w3id.org/ro/terms/earth-science#normScore 10.9375 https://w3id.org/ro-id/enrichment/918b5844-10ad-4297-9a29-f6230b3a0068 https://w3id.org/ro/terms/earth-science#score 7.7 https://w3id.org/ro-id/enrichment/93f13707-eae9-450a-a56a-a2943bafddd7 http://schema.org/name planet https://w3id.org/ro-id/enrichment/93f13707-eae9-450a-a56a-a2943bafddd7 http://www.w3.org/1999/02/22-rdf-syntax-ns#type https://w3id.org/ro/terms/earth-science#Lemma https://w3id.org/ro-id/enrichment/93f13707-eae9-450a-a56a-a2943bafddd7 https://w3id.org/ro/terms/earth-science#normScore 10.65340909090909 https://w3id.org/ro-id/enrichment/93f13707-eae9-450a-a56a-a2943bafddd7 https://w3id.org/ro/terms/earth-science#score 7.5 https://w3id.org/ro-id/enrichment/9c3ca068-4d17-408c-8d6e-185028903949 http://schema.org/name Arctic Zone https://w3id.org/ro-id/enrichment/9c3ca068-4d17-408c-8d6e-185028903949 http://www.w3.org/1999/02/22-rdf-syntax-ns#type https://w3id.org/contentdesc#Place https://w3id.org/ro-id/enrichment/9c3ca068-4d17-408c-8d6e-185028903949 https://w3id.org/ro/terms/earth-science#wikidata https://www.wikidata.org/wiki/Q25322 https://w3id.org/ro-id/enrichment/b64a2c92-2a3a-4e01-9fb3-92c90fa0b1ca http://schema.org/name Troms Fylke https://w3id.org/ro-id/enrichment/b64a2c92-2a3a-4e01-9fb3-92c90fa0b1ca http://www.w3.org/1999/02/22-rdf-syntax-ns#type https://w3id.org/ro/terms/earth-science#Lemma https://w3id.org/ro-id/enrichment/b64a2c92-2a3a-4e01-9fb3-92c90fa0b1ca https://w3id.org/ro/terms/earth-science#normScore 21.164772727272727 https://w3id.org/ro-id/enrichment/b64a2c92-2a3a-4e01-9fb3-92c90fa0b1ca https://w3id.org/ro/terms/earth-science#score 14.9 https://w3id.org/ro-id/enrichment/ba03a841-a1c7-4c34-8148-63a05e65f389 http://schema.org/name geophysics https://w3id.org/ro-id/enrichment/ba03a841-a1c7-4c34-8148-63a05e65f389 http://www.w3.org/1999/02/22-rdf-syntax-ns#type https://w3id.org/ro/terms/earth-science#NASA https://w3id.org/ro-id/enrichment/ba03a841-a1c7-4c34-8148-63a05e65f389 https://w3id.org/ro/terms/earth-science#normScore 100.0 https://w3id.org/ro-id/enrichment/ba03a841-a1c7-4c34-8148-63a05e65f389 https://w3id.org/ro/terms/earth-science#score 0.9452055096626282 https://w3id.org/ro-id/enrichment/bc45e45a-2976-4c72-a5dc-17e621dc74c0 http://schema.org/name brown in Troms https://w3id.org/ro-id/enrichment/bc45e45a-2976-4c72-a5dc-17e621dc74c0 http://www.w3.org/1999/02/22-rdf-syntax-ns#type https://w3id.org/ro/terms/earth-science#Phrase https://w3id.org/ro-id/enrichment/bc45e45a-2976-4c72-a5dc-17e621dc74c0 https://w3id.org/ro/terms/earth-science#normScore 10.314875135722042 https://w3id.org/ro-id/enrichment/bc45e45a-2976-4c72-a5dc-17e621dc74c0 https://w3id.org/ro/terms/earth-science#score 9.5 https://w3id.org/ro-id/enrichment/cf6d57b8-3cd9-4d03-b6a3-c1d8948d6229 http://schema.org/name environmental condition https://w3id.org/ro-id/enrichment/cf6d57b8-3cd9-4d03-b6a3-c1d8948d6229 http://www.w3.org/1999/02/22-rdf-syntax-ns#type https://w3id.org/ro/terms/earth-science#Concept https://w3id.org/ro-id/enrichment/cf6d57b8-3cd9-4d03-b6a3-c1d8948d6229 https://w3id.org/ro/terms/earth-science#normScore 3.3570701932858595 https://w3id.org/ro-id/enrichment/cf6d57b8-3cd9-4d03-b6a3-c1d8948d6229 https://w3id.org/ro/terms/earth-science#score 3.3 https://w3id.org/ro-id/enrichment/d3ac184c-6295-46f4-82ac-eab7301ac740 http://schema.org/name Norway https://w3id.org/ro-id/enrichment/d3ac184c-6295-46f4-82ac-eab7301ac740 http://www.w3.org/1999/02/22-rdf-syntax-ns#type https://w3id.org/contentdesc#Place https://w3id.org/ro-id/enrichment/d3ac184c-6295-46f4-82ac-eab7301ac740 https://w3id.org/ro/terms/earth-science#wikidata https://www.wikidata.org/wiki/Q20 https://w3id.org/ro-id/enrichment/e0e30393-3a62-4753-9f71-93c0c1cbbe5c http://schema.org/name greening Earth https://w3id.org/ro-id/enrichment/e0e30393-3a62-4753-9f71-93c0c1cbbe5c http://www.w3.org/1999/02/22-rdf-syntax-ns#type https://w3id.org/ro/terms/earth-science#Phrase https://w3id.org/ro-id/enrichment/e0e30393-3a62-4753-9f71-93c0c1cbbe5c https://w3id.org/ro/terms/earth-science#normScore 36.91639522258415 https://w3id.org/ro-id/enrichment/e0e30393-3a62-4753-9f71-93c0c1cbbe5c https://w3id.org/ro/terms/earth-science#score 34.0 https://w3id.org/ro-id/enrichment/e14b802d-423a-4d73-ac88-ac383c49ac1d http://schema.org/name counties in northern Norway https://w3id.org/ro-id/enrichment/e14b802d-423a-4d73-ac88-ac383c49ac1d http://www.w3.org/1999/02/22-rdf-syntax-ns#type https://w3id.org/ro/terms/earth-science#Phrase https://w3id.org/ro-id/enrichment/e14b802d-423a-4d73-ac88-ac383c49ac1d https://w3id.org/ro/terms/earth-science#normScore 5.320304017372422 https://w3id.org/ro-id/enrichment/e14b802d-423a-4d73-ac88-ac383c49ac1d https://w3id.org/ro/terms/earth-science#score 4.9 https://w3id.org/ro-id/enrichment/edc9a8ce-1ad1-4c9b-b4f6-bd42789cca35 http://schema.org/name Finnmark Fylke https://w3id.org/ro-id/enrichment/edc9a8ce-1ad1-4c9b-b4f6-bd42789cca35 http://www.w3.org/1999/02/22-rdf-syntax-ns#type https://w3id.org/contentdesc#Place https://w3id.org/ro-id/enrichment/edc9a8ce-1ad1-4c9b-b4f6-bd42789cca35 https://w3id.org/ro/terms/earth-science#wikidata https://www.wikidata.org/wiki/Q50632 https://w3id.org/ro-id/enrichment/ef9c7374-d8f1-4970-8171-fe2c8385e216 http://schema.org/name earth sciences https://w3id.org/ro-id/enrichment/ef9c7374-d8f1-4970-8171-fe2c8385e216 http://www.w3.org/1999/02/22-rdf-syntax-ns#type https://w3id.org/ro/terms/earth-science#FieldOfResearch https://w3id.org/ro-id/enrichment/ef9c7374-d8f1-4970-8171-fe2c8385e216 https://w3id.org/ro/terms/earth-science#normScore 100.0 https://w3id.org/ro-id/enrichment/ef9c7374-d8f1-4970-8171-fe2c8385e216 https://w3id.org/ro/terms/earth-science#score 0.7859669327735901 https://www-nature-com.ezproxy.uio.no/articles/s43017-022-00298-5 http://schema.org/author https://orcid.org/0000-0002-8763-1643 https://www-nature-com.ezproxy.uio.no/articles/s43017-022-00298-5 http://schema.org/contentUrl https://www-nature-com.ezproxy.uio.no/articles/s43017-022-00298-5 https://www-nature-com.ezproxy.uio.no/articles/s43017-022-00298-5 http://schema.org/creator https://orcid.org/0000-0002-8763-1643 https://www-nature-com.ezproxy.uio.no/articles/s43017-022-00298-5 http://schema.org/dateCreated 2022-10-19 12:47:23.064683+00:00 https://www-nature-com.ezproxy.uio.no/articles/s43017-022-00298-5 http://schema.org/dateModified 2022-10-19 12:47:23.578988+00:00 https://www-nature-com.ezproxy.uio.no/articles/s43017-022-00298-5 http://schema.org/description Vegetation indices (VIs), which describe remotely sensed vegetation properties such as photosynthetic activity and canopy structure, are widely used to study vegetation dynamics across scales. However, VI-based results can vary between indices, sensors, quality control measures, compositing algorithms, and atmospheric and sun–target–sensor geometry corrections. These variations make it difficult to draw robust conclusions about ecosystem change and highlight the need for consistent VI application and verification. In this Technical Review, we summarize the history and ecological applications of VIs and the linkages and inconsistencies between them. VIs have been used since the early 1970s and have evolved rapidly with the emergence of new satellite sensors with more spectral channels, new scientific demands and advances in spectroscopy. When choosing VIs, the spectral sensitivity and features of VIs and their suitability for target application should be considered. During data analyses, steps must be taken to minimize the impact of artefacts, VI results should be verified with in situ data when possible and conclusions should be based on multiple sets of indicators. Next-generation VIs with higher signal-to-noise ratios and fewer artefacts will be possible with new satellite missions and integration with emerging vegetation metrics such as solar-induced chlorophyll fluorescence, providing opportunities for studying terrestrial ecosystems globally. https://www-nature-com.ezproxy.uio.no/articles/s43017-022-00298-5 http://schema.org/keywords Vegetation indices https://www-nature-com.ezproxy.uio.no/articles/s43017-022-00298-5 http://schema.org/license https://choosealicense.com/no-permission/ https://www-nature-com.ezproxy.uio.no/articles/s43017-022-00298-5 http://schema.org/name Optical vegetation indices for monitoring terrestrial ecosystems globally https://www-nature-com.ezproxy.uio.no/articles/s43017-022-00298-5 http://schema.org/sdDatePublished 2022-10-19 12:47:23.064683+00:00 https://www-nature-com.ezproxy.uio.no/articles/s43017-022-00298-5 http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://purl.org/wf4ever/wf4ever#Resource https://www-nature-com.ezproxy.uio.no/articles/s43017-022-00298-5 http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://schema.org/Article https://www-nature-com.ezproxy.uio.no/articles/s43017-022-00298-5 http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://schema.org/MediaObject https://www.sciencedirect.com/science/article/pii/S1873965213000455 http://schema.org/author https://orcid.org/0000-0002-8763-1643 https://www.sciencedirect.com/science/article/pii/S1873965213000455 http://schema.org/contentUrl https://www.sciencedirect.com/science/article/pii/S1873965213000455 https://www.sciencedirect.com/science/article/pii/S1873965213000455 http://schema.org/creator https://orcid.org/0000-0002-8763-1643 https://www.sciencedirect.com/science/article/pii/S1873965213000455 http://schema.org/dateCreated 2023-05-25 06:37:48.986995+00:00 https://www.sciencedirect.com/science/article/pii/S1873965213000455 http://schema.org/dateModified 2023-05-25 06:37:51.001310+00:00 https://www.sciencedirect.com/science/article/pii/S1873965213000455 http://schema.org/description Abstract Droppings of Svalbard reindeer (Rangifer tarandus platyrhynchus) could affect the carbon and nitrogen cycles in tundra ecosystems. The aim of this study was to evaluate the potential of reindeer droppings originating from the winter diet for emission and/or absorption of methane (CH4) and nitrous oxide (N2O) in summer. An incubation experiment was conducted over 14 days using reindeer droppings and mineral subsoil collected from a mound near Ny-Ålesund, Svalbard, to determine the potential exchanges of CH4 and N2O for combinations of two factors, reindeer droppings (presence or absence) and soil moisture (dry, moderate, or wet). A line transect survey was conducted to determine the distribution density of winter droppings at the study site. The incubation experiment showed a weak absorption of CH4 and a weak emission of N2O. Reindeer droppings originating from the winter diet had a negligible effect on the exchange fluxes of both CH4 and N2O. Although the presence of droppings resulted in a short-lasting increase in N2O emissions on day 1 (24 h from the start) for moderate and wet conditions, the emission rates were still very small, up to 3 μg N2O m−2 h−1. https://www.sciencedirect.com/science/article/pii/S1873965213000455 http://schema.org/keywords Reindeer https://www.sciencedirect.com/science/article/pii/S1873965213000455 http://schema.org/keywords droppings https://www.sciencedirect.com/science/article/pii/S1873965213000455 http://schema.org/keywords lichen https://www.sciencedirect.com/science/article/pii/S1873965213000455 http://schema.org/license https://choosealicense.com/no-permission/ https://www.sciencedirect.com/science/article/pii/S1873965213000455 http://schema.org/name Potential of Svalbard reindeer winter droppings for emission/absorption of methane and nitrous oxide during summer https://www.sciencedirect.com/science/article/pii/S1873965213000455 http://schema.org/sdDatePublished 2023-05-25 06:37:48.986995+00:00 https://www.sciencedirect.com/science/article/pii/S1873965213000455 http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://purl.org/wf4ever/roterms#Paper https://www.sciencedirect.com/science/article/pii/S1873965213000455 http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://purl.org/wf4ever/wf4ever#Resource https://www.sciencedirect.com/science/article/pii/S1873965213000455 http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://schema.org/MediaObject mailto:service-account-enrichment http://schema.org/name service-account-enrichment mailto:service-account-enrichment http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://xmlns.com/foaf/0.1/Agent https://w3id.org/np/RAP2P7SYOHe23ItJJmcFm0BASk2pcIZLfkpByaqz0eBDo/provenance https://w3id.org/np/RAP2P7SYOHe23ItJJmcFm0BASk2pcIZLfkpByaqz0eBDo/assertion http://www.w3.org/ns/prov#wasDerivedFrom https://api.rohub.org/api/ros/3ed30e69-fb38-4045-bd34-2fa907d12353/crate/download/ro-crate-metadata.json https://w3id.org/np/RAP2P7SYOHe23ItJJmcFm0BASk2pcIZLfkpByaqz0eBDo/pubinfo https://w3id.org/np/RAP2P7SYOHe23ItJJmcFm0BASk2pcIZLfkpByaqz0eBDo http://purl.org/dc/terms/created 2025-11-11T16:28:28.994+01:00 https://w3id.org/np/RAP2P7SYOHe23ItJJmcFm0BASk2pcIZLfkpByaqz0eBDo http://purl.org/nanopub/x/introduces https://w3id.org/ro-id/3ed30e69-fb38-4045-bd34-2fa907d12353/ https://w3id.org/np/RAP2P7SYOHe23ItJJmcFm0BASk2pcIZLfkpByaqz0eBDo http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://purl.org/nanopub/x/RoCrateNanopub https://w3id.org/np/RAP2P7SYOHe23ItJJmcFm0BASk2pcIZLfkpByaqz0eBDo http://www.w3.org/2000/01/rdf-schema#label Vegetation browning in Troms and Finnmark (Norway) https://w3id.org/np/RAP2P7SYOHe23ItJJmcFm0BASk2pcIZLfkpByaqz0eBDo/sig http://purl.org/nanopub/x/hasAlgorithm RSA https://w3id.org/np/RAP2P7SYOHe23ItJJmcFm0BASk2pcIZLfkpByaqz0eBDo/sig http://purl.org/nanopub/x/hasPublicKey MIIBIjANBgkqhkiG9w0BAQEFAAOCAQ8AMIIBCgKCAQEA4pPaESKwmC6l37P86K6TNLq6yeQtc7m9CvcqauLs/1FC0viHvQnFBgxj0a+loPDv/Egwe6OqFpa0iW9Ypnyz9YPoh+pxbRXonbuMOb+8Ry9hXZ+TEKfWjhjVDGEaClwfRwglh2HI/xfV4CD9AgvDOEoZQiyta8a90PYwJ3G6e70oCHTn61+OWTkI9KRYHOYgg3btdy2Z7q/30PTFawb2ZT5aIfIJYobUYv2a7yhtcqWCHZeKv0bxGnRjTFNx1rscBMlLJSzvRtpQc1cCRVEPFZHo1adaXCI9tGvn4cxeNQ96y8dxkN1XhpaJairde+23MDzf42Oe97KG2HYzKiyVnQIDAQAB https://w3id.org/np/RAP2P7SYOHe23ItJJmcFm0BASk2pcIZLfkpByaqz0eBDo/sig http://purl.org/nanopub/x/hasSignature rliFl5KAPltehKLaaWwubkXdGMRbGn1kVTLfvn1YCvFIC4LKJo7hwFdz66p+ocju4WeivMlshy2xdQEllIS+gm653cedR7LXoRul9wMzgVP9Nyr9NmR4V1WxPxZEY10MACpfnq8PX7iAKymU73ZE3hICz3CHIt61c9Qk0JAAgHZFakIsV+Moy1ZfZ5H0mo0rgUlnQCpbu4lVgajLDYWnB+NHJdLmU8eHIowh+Dg+jgikSSH9kMP4+JAmUgh3BsD/5AJ2/rQqnMl3Kjeh9VHBXREifSq/Ic84hOCdu0P0CYhzMkZ9mrqG/mh7NyKMseQO7oZvlq2iCJZXy8NmFib46g== https://w3id.org/np/RAP2P7SYOHe23ItJJmcFm0BASk2pcIZLfkpByaqz0eBDo/sig http://purl.org/nanopub/x/hasSignatureTarget https://w3id.org/np/RAP2P7SYOHe23ItJJmcFm0BASk2pcIZLfkpByaqz0eBDo https://w3id.org/np/RAP2P7SYOHe23ItJJmcFm0BASk2pcIZLfkpByaqz0eBDo/sig http://purl.org/nanopub/x/signedBy https://w3id.org/kpxl/gen/terms/RoCrateBot