Zobrazeno 1 - 10
of 162
pro vyhledávání: '"T. Salles"'
Autor:
S. Polanco, M. Blum, T. Salles, B. C. Frederick, R. Farrington, X. Ding, B. Mather, C. Mallard, L. Moresi
Publikováno v:
Earth Surface Dynamics, Vol 12, Pp 301-320 (2024)
The interplay between climate-forced sea level change, erosional and depositional processes, and flexural isostasy in deep time on passive margin deltas remains poorly understood. We performed a series of conceptual simulations to investigate flexura
Externí odkaz:
https://doaj.org/article/2a5a045271e441dc92ab18661a78a228
Publikováno v:
Earth Surface Dynamics, Vol 11, Pp 183-201 (2023)
Detrital 10Be from continental river sands or submarine sediments has been extensively used to determine the average long-term denudation rates of terrestrial catchments, based on the assumption that the rate of cosmogenic nuclide production by the i
Externí odkaz:
https://doaj.org/article/58921f52aa8245639e7bba71a4e78273
Autor:
G. Brocard, J. K. Willenbring, T. Salles, M. Cosca, A. Guttiérez-Orrego, N. Cacao Chiquín, S. Morán-Ical, C. Teyssier
Publikováno v:
Earth Surface Dynamics, Vol 9, Pp 795-822 (2021)
The rise of a mountain range affects moisture circulation in the atmosphere and water runoff across the land surface, modifying the distribution of precipitation and drainage patterns in its vicinity. Water routing in turn affects erosion on hillslop
Externí odkaz:
https://doaj.org/article/79c6045a3f334649a4df425af94fdfea
Publikováno v:
Earth Surface Dynamics, Vol 7, Pp 895-910 (2019)
Species distribution and richness ultimately result from complex interactions between biological, physical, and environmental factors. It has been recently shown for a static natural landscape that the elevational connectivity, which measures the pro
Externí odkaz:
https://doaj.org/article/3faa501352044d15868000d725cc376c
Autor:
T. Salles
Publikováno v:
Geoscientific Model Development, Vol 12, Pp 4165-4184 (2019)
The eSCAPE model is a Python-based landscape evolution model that simulates over geological time (1) the dynamics of the landscape, (2) the transport of sediment from source to sink, and (3) continental and marine sedimentary basin formation under di
Externí odkaz:
https://doaj.org/article/65e6119d00ad4f61b2cd15f0a5fef9bd
Publikováno v:
Geoscientific Model Development, Vol 12, Pp 2571-2585 (2019)
The sedimentary architecture at continental margins reflects the interplay between the rate of change of accommodation creation (δA) and the rate of change of sediment supply (δS). Stratigraphic interpretation increasingly focuses on understanding
Externí odkaz:
https://doaj.org/article/7d1a985f1d334a52a5b3e0a8f230bf3f
Publikováno v:
Frontiers in Earth Science, Vol 8 (2020)
As anthropogenic forcing continues to rapidly modify worldwide climate, impacts on landscape changes will grow. Olivine weathering is a natural process that sequesters carbon out of the atmosphere, but is now being proposed as a strategy that can be
Externí odkaz:
https://doaj.org/article/598a493d7d9e47af9d7c1aa028bb5ef5
Publikováno v:
Geoscientific Model Development, Vol 11, Pp 2093-2110 (2018)
Assemblages of corals characterise specific reef biozones and the environmental conditions that change spatially across a reef and with depth. Drill cores through fossil reefs record the time and depth distribution of assemblages, which captures a
Externí odkaz:
https://doaj.org/article/5fcd46dc272941cf8679e3eb14c9b0d2
Autor:
T. Salles
Publikováno v:
SoftwareX, Vol 5, Iss , Pp 195-202 (2016)
Over more than three decades, a number of numerical landscape evolution models (LEMs) have been developed to study the combined effects of climate, sea-level, tectonics and sediments on Earth surface dynamics. Most of them are written in efficient pr
Externí odkaz:
https://doaj.org/article/00f80ade19844f779362458ca1c0379e
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