Matches in Nanopublications for { ?s ?p ?o <https://w3id.org/np/RAP2P7SYOHe23ItJJmcFm0BASk2pcIZLfkpByaqz0eBDo/assertion>. }
- a813607d-29ac-4e73-84c2-ee23315be103 description "Poster presented at EGU 2023 during the ESSI2.8 "HPC and cloud infrastructures in support of Earth Observation, Earth Modeling and community-driven Geoscience approach PANGEO" Convener: Vasileios Baousis | Co-conveners: Tina Odaka, Umberto Modigliani, Anne Fouilloux, Alejandro Coca-CastroECS" assertion.
- d2502da9-7821-4443-84fc-fdf20dd120c9 description "This poster shows the work done to estimate the loss in lichens & mosses in the arctic (arctic browning). ERA5 land data from ECMWF have been used to estimate the changes in vegetation. Poster in svg format that has been presented at EGU 2023 at session ESSI2.8 HPC and cloud infrastructures in support of Earth Observation, Earth Modeling and community-driven Geoscience approach PANGEO Convener: Vasileios Baousis | Co-conveners: Tina Odaka, Umberto Modigliani, Anne Fouilloux, Alejandro Coca-Castro" assertion.
- j.jhydrol.2022.128593 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." assertion.
- 1550592 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." assertion.
- egusphere-egu23-2579 description "Summary submitted at EGU 2023." assertion.
- train_mooc_tp1n.ipynb description "Jupyter Notebook for training, testing and validating machine learning method to forecast moss and lichen fractional cover mean. This Jupyter Notebook uses Python and Keras." assertion.
- S1873965213000455 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." assertion.
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