Zobrazeno 1 - 10
of 75
pro vyhledávání: '"A. Mark Jellinek"'
Autor:
Shawn M. Chartrand, A. Mark Jellinek, Antero Kukko, Anna Grau Galofre, Gordon R. Osinski, Shannon Hibbard
Publikováno v:
Nature Communications, Vol 14, Iss 1, Pp 1-12 (2023)
Abstract Stream networks in Arctic and high-elevation regions underlain by frozen ground (i.e., permafrost) are expanding and developing in response to accelerating global warming, and intensifying summertime climate variability. The underlying proce
Externí odkaz:
https://doaj.org/article/cb334d0909f347ba963d16ed2d02bf9f
Autor:
Thomas J. Aubry, Samantha L. Engwell, Costanza Bonadonna, Larry G. Mastin, Guillaume Carazzo, Alexa R. VanEaton, David E. Jessop, Roy G. Grainger, Simona Scollo, Isabelle A. Taylor, A. Mark Jellinek, Anja Schmidt, Sébastien Biass, Mathieu Gouhier
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 14, Pp n/a-n/a (2023)
Abstract Rapid and simple estimation of the mass eruption rate (MER) from column height is essential for real‐time volcanic hazard management and reconstruction of past explosive eruptions. Using 134 eruptive events from the new Independent Volcani
Externí odkaz:
https://doaj.org/article/86f5743a16dd43e29ec3c9f25e34fb08
Publikováno v:
Frontiers in Earth Science, Vol 10 (2022)
Explosive volcanic eruptions can inject sulfur dioxide (SO2) into the stratosphere to form aerosol particles that modify Earth’s radiation balance and drive surface cooling. Eruptions involving interactions with shallow layers (≤500 m) of surface
Externí odkaz:
https://doaj.org/article/b7de847041b64589bc88f068d6cfaad8
Publikováno v:
Nature Geoscience. 16:446-453
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::19edb017947a8814f687f608e9e7609f
https://doi.org/10.1038/s41561-023-01160-z
https://doi.org/10.1038/s41561-023-01160-z
Publikováno v:
Earth Surface Dynamics. 11:1-20
A potential control of downstream channel width variations on the structure and planform of pool–riffle sequence local bed topography is a key to the dynamics of gravel bed rivers. How established pool–riffle sequences respond to time-varying cha
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::458df3b61431f00c9cc3b8334b342fac
https://doi.org/10.5194/esurf-11-1-2023
https://doi.org/10.5194/esurf-11-1-2023
Volcanic plumes typically have unsteady source conditions, where mass and heat fluxes from the vent evolve or fluctuate on time scales from seconds to hours. However, integral plume models routinely assume source conditions that are statistically sta
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5374b05893faf6901928638c6363a56c
https://doi.org/10.22541/essoar.167810132.29360847/v1
https://doi.org/10.22541/essoar.167810132.29360847/v1
Autor:
Thomas Jacques Aubry, Samantha L Engwell, Costanza Bonadonna, Larry Garver Mastin, Guillaume Carazzo, Alexa Van Eaton, David Jessop, Roy Gordon Grainger, Simona Scollo, Isabelle Alice Taylor, Mark Jellinek, Anja Schmidt, Sébastien Biass, Mathieu Gouhier
Relating the mass eruption rate (MER) of explosive eruptions to column height in the atmosphere is key to reconstructing past eruptions and forecasting volcanic hazards. Using 134 eruptive events from the Independent Volcanic Eruption Source Paramete
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4cbb030b4944b0f7197928ede8426725
https://uca.hal.science/hal-03917579
https://uca.hal.science/hal-03917579
Catastrophic caldera-forming (CCF) eruptions are the most impressive of volcanic phenomena in the geological record. Regionally, ash fall, pyroclastic density currents (PDCs), and tsunamis during such events can devastate civilizations and have power
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b408105e522131c8a8bb3d21153034f9
https://doi.org/10.21203/rs.3.rs-2140664/v1
https://doi.org/10.21203/rs.3.rs-2140664/v1
A potential control of downstream channel width variations on the structure and planform of pool-riffle sequence local bed topography is a key to the dynamics of gravel-bed rivers. How established pool-riffle sequences respond to time-varying shifts
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::db7dcffa30cd35001b0d193530ee853e
https://doi.org/10.5194/esurf-2022-40
https://doi.org/10.5194/esurf-2022-40