scholarly journals Role of low-latitude forests in modulating forest filter effect on a continental scale: Long-term simulation on PCB-153 in Chinese forests

2021 ◽  
Vol 778 ◽  
pp. 146285
Author(s):  
Yue Xu ◽  
Chongguo Tian ◽  
Luca Nizzetto ◽  
Gan Zhang
2013 ◽  
Vol 74 ◽  
pp. 378-384 ◽  
Author(s):  
Elisa Terzaghi ◽  
Edward Wild ◽  
Gabriele Zacchello ◽  
Bruno E.L. Cerabolini ◽  
Kevin C. Jones ◽  
...  

2018 ◽  
Author(s):  
Stefan Hergarten ◽  
Thomas Kenkmann

Abstract. Worldwide erosion rates seem to have increased strongly since the beginning of the Quaternary, but there is still discussion about the role of glaciation as a potential driver and even whether the increase is real at all or an artefact due to losses in the long-term sedimentary record. In this study we derive estimates of average erosion rates on the time scale of some tens of million years from the terrestrial impact crater inventory. This approach is completely independent from all other methods to infer erosion rates such as river loads, preserved sediments, cosmogenic nuclides and thermochronometry. Our approach yields average erosion rates as a function of present-day topography and climate. The results confirm that topography accounts for the main part of the huge variation of erosion on Earth, but also identifies a significant systematic dependence on climate in contrast to several previous studies. We found a fivefold increase in erosional efficacy from the cold regimes to the tropical zone and that temperate and arid climates are very similar in this context. Combining our results to a worldwide mean erosion rate we found that erosion rates on the time scale of some tens of million years are at least as high as present-day rates and suggest that glaciation has a rather regional effect with a limited impact at the continental scale.


2019 ◽  
Vol 7 (2) ◽  
pp. 459-473 ◽  
Author(s):  
Stefan Hergarten ◽  
Thomas Kenkmann

Abstract. Worldwide erosion rates seem to have increased strongly since the beginning of the Quaternary, but there is still discussion about the role of glaciation as a potential driver and even whether the increase is real at all or an artifact due to losses in the long-term sedimentary record. In this study we derive estimates of average erosion rates on the timescale of some tens of millions of years from the terrestrial impact crater inventory. This approach is completely independent from all other methods to infer erosion rates such as river loads, preserved sediments, cosmogenic nuclides, and thermochronometry. Our approach yields average erosion rates as a function of present-day topography and climate. The results confirm that topography accounts for the main part of the huge variation in erosion on Earth, but also identifies a significant systematic dependence on climate in contrast to several previous studies. We found a 5-fold increase in erosional efficacy from the cold regimes to the tropical zone and that temperate and arid climates are very similar in this context. Combining our results into a worldwide mean erosion rate, we found that erosion rates on the timescale of some tens of millions of years are at least as high as present-day rates and suggest that glaciation has a rather regional effect with a limited impact at the continental scale.


2003 ◽  
Vol 17 (4) ◽  
pp. 244-248 ◽  
Author(s):  
F. Wegmann ◽  
M. Scheringer ◽  
M. M�ller ◽  
K. Hungerb�hler

2014 ◽  
Vol 121 ◽  
pp. 168-176 ◽  
Author(s):  
M. Venkat Ratnam ◽  
N. Venkateswara Rao ◽  
C. Vedavathi ◽  
B.V. Krishna Murthy ◽  
S. Vijaya Bhaskara Rao

2006 ◽  
Vol 63 (1) ◽  
pp. 75-83 ◽  
Author(s):  
Luca Nizzetto ◽  
Chiara Cassani ◽  
Antonio Di Guardo

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