Zonobiome of the Cold-Temperate Boreal Climate

Author(s):  
Heinrich Walter
Keyword(s):  
2013 ◽  
Vol 17 (1) ◽  
pp. 325-339 ◽  
Author(s):  
C. Schneider ◽  
C. L. R. Laizé ◽  
M. C. Acreman ◽  
M. Flörke

Abstract. Worldwide, flow regimes are being modified by various anthropogenic impacts and climate change induces an additional risk. Rising temperatures, declining snow cover and changing precipitation patterns will interact differently at different locations. Consequently, in distinct climate zones, unequal consequences can be expected in matters of water stress, flood risk, water quality, and food security. In particular, river ecosystems and their vital ecosystem services will be compromised as their species richness and composition have evolved over long time under natural flow conditions. This study aims at evaluating the exclusive impacts of climate change on river flow regimes in Europe. Various flow characteristics are taken into consideration and diverse dynamics are identified for each distinct climate zone in Europe. In order to simulate present-day natural flow regimes and future flow regimes under climate change, the global hydrology model WaterGAP3 is applied. All calculations for current and future conditions (2050s) are carried out on a 5' × 5' European grid. To address uncertainty, bias-corrected climate forcing data of three different global climate models are used to drive WaterGAP3. Finally, the hydrological alterations of different flow characteristics are quantified by the Indicators of Hydrological Alteration approach. Results of our analysis indicate that on the European scale, climate change can be expected to modify flow regimes remarkably. This is especially the case in the Mediterranean (due to drier conditions with reduced precipitation across the year) and in the boreal climate zone (due to reduced snowmelt, increased precipitation, and strong temperature rises). In the temperate climate zone, impacts increase from oceanic to continental. Regarding single flow characteristics, strongest impacts on timing were found for the boreal climate zone. This applies for both high and low flows. Flow magnitudes, in turn, will be predominantly altered in the Mediterranean but also in the Northern climates. At the end of this study, typical future flow regimes under climate change are illustrated for each climate zone.


Palynology ◽  
2014 ◽  
Vol 39 (1) ◽  
pp. 91-102 ◽  
Author(s):  
Matthew J. Pound ◽  
Robert I. Lowther ◽  
Jeff Peakall ◽  
Robert J. Chapman ◽  
Ulrich Salzmann

Author(s):  
Forrest G. Hall ◽  
Alan K. Betts ◽  
Steve Frolking ◽  
Ross Brown ◽  
Jing M. Chen ◽  
...  
Keyword(s):  

Ecosystems ◽  
2015 ◽  
Vol 18 (6) ◽  
pp. 1014-1028 ◽  
Author(s):  
Mathilde Chomel ◽  
Marie Guittonny-Larchevêque ◽  
Annie DesRochers ◽  
Virginie Baldy

2020 ◽  
Vol 170 (3) ◽  
pp. 440-450
Author(s):  
Muhammad Nadeem ◽  
Raymond Thomas ◽  
Oludoyin Adigun ◽  
Charles Manful ◽  
Jiaxu Wu ◽  
...  

2015 ◽  
Vol 532 ◽  
pp. 752-761 ◽  
Author(s):  
Lijuan Yan ◽  
Petri Penttinen ◽  
Asko Simojoki ◽  
Frederick L. Stoddard ◽  
Kristina Lindström

1988 ◽  
Vol 66 (12) ◽  
pp. 2424-2430 ◽  
Author(s):  
A. G. Schwarz ◽  
R. E. Redmann

Six C4 grasses (Distichlis stricta, Muhlenbergia glomerata var. cinnoides, M. mexicana, M. richardsonis, Spartina gracilis, S. pectinata) were found in grassy openings in the boreal forest of northwestern Canada. High carbon isotope ratios and Kranz anatomy confirmed that these northern populations are functionally C4 grasses. Muhlenbergia mexicana was assumed to be a C4 grass on the basis of published data. Recent collections of C4 plants tended to have more negative δ13C values than older collections from northern locations, which may reflect decreases in δ13C of atmospheric CO2 over time. In general, northern C4 species had lower δ13C values than those reported for their southern counterparts. The boreal climate in the north supports C4 species only where the mean minimum temperature for July is at least 7.5 °C. C4 grasses were found in microsites warmed by high irradiance or geothermal activity; many of the sites had saline substrates. Northern C4 populations are rare and unique in the boreal flora and deserve special protection.


2004 ◽  
Vol 34 (7) ◽  
pp. 1369-1378 ◽  
Author(s):  
Martin Weih

Short rotation forestry (SRF) is regarded as a silvicultural practice employing high-density plantations of fast-growing tree species on fertile land with a rotation period of fewer than 10–12 years. I address the challenges and possibilities of SRF applications under the circumstances of a boreal climate, today as well as after anticipated climate change. The implications of a pronounced winter season for the performance of biomass crops are discussed. Poplars, aspens, and willows are superior in boreal SRF because of their fast growth rate in combination with good cold hardiness. These trees can enrich the coniferous forests of boreal regions and increase biodiversity in open agricultural landscapes of the boreal zone. Further, SRF plantations can serve as tools for the amelioration of environmental problems at local (e.g., phytoremediation) and global (e.g., increased greenhouse effect) scales. The biomass yields achieved in boreal SRF and the appropriate production systems appear do not appear to be principally different from warmer regions, but there are some differences with respect to the importance of fertilization, appropriate spacing, and rotation length. The major barriers for a rapid development of SRF appear not to be climatic, technical, or environmental constraints in many boreal regions.


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