Environmental evidence of Valencia Lagoon coastal barrier stabilization from 8500 BP to Present. Climate and eustatic variations

Author(s):  
M. López-Belzunce ◽  
A.M. Blázquez ◽  
Y. Sánchez-Palencia ◽  
T. Torres ◽  
J.E. Ortiz
2009 ◽  
Vol 160 (3) ◽  
pp. 68-73 ◽  
Author(s):  
Jean-Philippe Schütz

Since the present climate in Switzerland includes abundant rainfall, the climatic changes should not present any serious danger of the ground drying out. In fact, higher precipitation levels are predicted. So it would seem that climate is likely to become more luxuriant rather than more dry. These conditions – together with the entry of nutrients with the rainfall – favour the growth of ash and maple but not of oak. Even with an increase in stressful dry summer periods, a consideration of the broad areas of distribution of indigenous species shows they possess a sufficiently great adaptability. Research into the effects of physiological stress on fir trees from different provenances shows in particular that those with local origins are better adapted to the habitat than those from elsewhere. The danger of an increase in storms should be countered by strategies aimed at increased resistance – through mixed plantation regulation and thinning out – rather than avoidance strategies. Ecoforestry is basically well armed for this task. It should be even more orientated towards the adaptability and resilience of forests.


2019 ◽  
Vol 23 (4) ◽  
pp. 1867-1883 ◽  
Author(s):  
Igor Pavlovskii ◽  
Masaki Hayashi ◽  
Daniel Itenfisu

Abstract. Snowpack accumulation and depletion are important elements of the hydrological cycle in the Canadian prairies. The surface runoff generated during snowmelt is transformed into streamflow or fills numerous depressions driving the focussed recharge of groundwater in this dry setting. The snowpack in the prairies can undergo several cycles of accumulation and depletion in a winter. The timing of the melt affects the mechanisms of snowpack depletion and their hydrological implications. The effects of midwinter melts were investigated at four instrumented sites in the Canadian prairies. Unlike net radiation-driven snowmelt during spring melt, turbulent sensible heat fluxes were the dominant source of energy inputs for midwinter melt occurring in the period with low solar radiation inputs. Midwinter melt events affect several aspects of hydrological cycle with lower runoff ratios than subsequent spring melt events, due to their role in the timing of the focussed recharge. Remote sensing data have shown that midwinter melt events regularly occur under the present climate throughout the Canadian prairies, indicating applicability of the study findings throughout the region.


2004 ◽  
Vol 57 (3) ◽  
pp. 253-258
Author(s):  
RICHARD D. RHEINHARDT ◽  
MARTHA CRAIG RHEINHARDT

2004 ◽  
Vol 57 (3) ◽  
pp. 253 ◽  
Author(s):  
Richard D. Rheinhardt ◽  
Martha Craig Rheinhardt

1997 ◽  
Vol 3 (1) ◽  
pp. 9-18 ◽  
Author(s):  
H. J. van Wijnen ◽  
J. P. Bakker ◽  
Y. de Vries

2012 ◽  
pp. 198-261
Author(s):  
Jonathan Cowie
Keyword(s):  

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