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pro vyhledávání: '"Roberts, GG"'
\ud Successful inverse modeling of observed longitudinal river profiles suggests that fluvial landscapes are responsive to continent-wide tectonic forcing. However, inversion algorithms make simplifying assumptions about landscape erodibility and dra
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::221a084dbe43a6418b60f352a127c8f2
Disentangling contributions from environmental variables is crucial for explaining global biodiversity patterns. We use wavelet power spectra to separate wavelength-dependent trends across Earth’s surface. Spectra reveal scale- and location-depende
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1032::3d3cb954a4bc39f9695db939d5790207
http://hdl.handle.net/10044/1/97702
http://hdl.handle.net/10044/1/97702
A range of complex hydraulic and geomorphic processes shape terrestrial landscapes. It remains unclear how these processes act to generate observed drainage networks across scales of interest. To address this issue, we transform observed and syntheti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cbcd1eafb08e5a50129e49a28c02c4c9
In actively deforming regions fluvial systems are strongly regulated by uplift. River geometries record histories of vertical motions that can be used to examine the driving forces generating topographic relief. Iceland's rapidly evolving landscapes
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1032::2ebba4a97017328a47a1bdb5e7b9f123
http://hdl.handle.net/10044/1/65585
http://hdl.handle.net/10044/1/65585
Geological observations that constrain the history of mantle convection are sparse despite its importance in determining vertical and horizontal plate motions, plate rheology, and magmatism. We use a suite of geological and geophysical observations f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1032::cca4a26e47b3b8f8e7925a61176cb028
http://hdl.handle.net/10044/1/44561
http://hdl.handle.net/10044/1/44561
Mountain forests are subject to high rates of physical erosion which can export particulate nitrogen from ecosystems. However, the impact of geomorphic processes on nitrogen budgets remains poorly constrained. We have used the elemental and isotopic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1032::533551ca10a3cdebba86f7937113fc70
http://hdl.handle.net/10044/1/49552
http://hdl.handle.net/10044/1/49552
It is generally agreed that a region encompassing the Colorado Plateau has been uplifted by sub-crustal processes. Admittance calculations, tomographic studies and receiver function analyses suggest that dynamic support is generated by some combinati
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1032::2abff84e85b98bb770b172f6496c492b
http://hdl.handle.net/10044/1/49621
http://hdl.handle.net/10044/1/49621
We present a strategy for calculating uplift rates as a function of space and time from large sets oflongitudinal river profiles. This strategy assumes that the shape of a river profile is controlled by thehistory of uplift rate and moderated by the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1032::e82b23a123ed6816bcb6f5d3633e3a03
http://hdl.handle.net/10044/1/49602
http://hdl.handle.net/10044/1/49602
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