scholarly journals Site Dependence of Fluvial Incision Rate Scaling With Timescale

Author(s):  
Ron Nativ ◽  
Jens M. Turowski
2016 ◽  
Author(s):  
Junsheng Nie ◽  
◽  
Weitao Wang ◽  
Weitao Wang ◽  
Kerry Gallagher ◽  
...  

2021 ◽  
pp. 103476
Author(s):  
Willem Viveen ◽  
Jorge Sanjurjo-Sanchez ◽  
Patrice Baby ◽  
Maria del Rosario González-Moradas

Geomorphology ◽  
2021 ◽  
pp. 107665
Author(s):  
Thibaut Cardinal ◽  
Laurence Audin ◽  
Yann Rolland ◽  
Stéphane Schwartz ◽  
Carole Petit ◽  
...  
Keyword(s):  

2018 ◽  
Vol 22 (6) ◽  
pp. 3175-3196 ◽  
Author(s):  
Mathieu Vrac

Abstract. Climate simulations often suffer from statistical biases with respect to observations or reanalyses. It is therefore common to correct (or adjust) those simulations before using them as inputs into impact models. However, most bias correction (BC) methods are univariate and so do not account for the statistical dependences linking the different locations and/or physical variables of interest. In addition, they are often deterministic, and stochasticity is frequently needed to investigate climate uncertainty and to add constrained randomness to climate simulations that do not possess a realistic variability. This study presents a multivariate method of rank resampling for distributions and dependences (R2D2) bias correction allowing one to adjust not only the univariate distributions but also their inter-variable and inter-site dependence structures. Moreover, the proposed R2D2 method provides some stochasticity since it can generate as many multivariate corrected outputs as the number of statistical dimensions (i.e., number of grid cell  ×  number of climate variables) of the simulations to be corrected. It is based on an assumption of stability in time of the dependence structure – making it possible to deal with a high number of statistical dimensions – that lets the climate model drive the temporal properties and their changes in time. R2D2 is applied on temperature and precipitation reanalysis time series with respect to high-resolution reference data over the southeast of France (1506 grid cell). Bivariate, 1506-dimensional and 3012-dimensional versions of R2D2 are tested over a historical period and compared to a univariate BC. How the different BC methods behave in a climate change context is also illustrated with an application to regional climate simulations over the 2071–2100 period. The results indicate that the 1d-BC basically reproduces the climate model multivariate properties, 2d-R2D2 is only satisfying in the inter-variable context, 1506d-R2D2 strongly improves inter-site properties and 3012d-R2D2 is able to account for both. Applications of the proposed R2D2 method to various climate datasets are relevant for many impact studies. The perspectives of improvements are numerous, such as introducing stochasticity in the dependence itself, questioning its stability assumption, and accounting for temporal properties adjustment while including more physics in the adjustment procedures.


2009 ◽  
Vol 47 (1) ◽  
Author(s):  
L. Telesca ◽  
G. Colangelo ◽  
V. Lapenna ◽  
M. Macchiato
Keyword(s):  

2016 ◽  
Vol 86 (3) ◽  
pp. 326-334 ◽  
Author(s):  
Hongshan Gao ◽  
Zongmeng Li ◽  
Yapeng Ji ◽  
Baotian Pan ◽  
Xiaofeng Liu

AbstractThe Weihe River in central China is the largest tributary of the Yellow River and contains a well-developed strath terrace system. A new chronology for the past 1.11 Ma for a spectacular flight of strath terraces along the upper Weihe River near Longxi is defined based on field investigations of loess—paleosol sequences and magnetostratigraphy. All the strath terraces are strikingly similar, having several meters of paleosols that have developed directly on top of fluvial deposits located on the terrace treads. This suggests that the abandonment of each strath terrace by river incision occurred during the transition from glacial to interglacial climates. The average fluvial incision rates during 1.11—0.71 Ma and since 0.13 Ma are 0.35 and 0.32 m/ka, respectively. These incision rates are considerably higher than the average incision rate of 0.16 m/km for the intervening period between 0.71 and 0.13 Ma. Over all our results suggest that cyclic Quaternary climate change has been the main driving factor for strath terrace formation with enhanced episodic uplift.


1991 ◽  
Vol 81 (6) ◽  
pp. 2486-2492
Author(s):  
J. Morales ◽  
J. M. Ibáñez ◽  
F. Vidal ◽  
F. de Miguel ◽  
G. Alguacil ◽  
...  

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