Long-term temporal changes in central European tree phenology (1946−2010) confirm the recent extension of growing seasons

2014 ◽  
Vol 58 (8) ◽  
pp. 1739-1748 ◽  
Author(s):  
Eva Kolářová ◽  
Jiří Nekovář ◽  
Peter Adamík
Forests ◽  
2021 ◽  
Vol 12 (12) ◽  
pp. 1656
Author(s):  
Petr Kupec ◽  
Jan Deutscher ◽  
Martyn Futter

In this study, we present evidence for a hydrological regime shift in upland central European forests. Using a combination of long-term data, detailed field measurements and modelling, we show that there is a prolonged and persistent decline in annual runoff: precipitation ratios that is most likely linked to longer growing seasons. We performed a long term (1950–2018) water balance simulation for a Czech upland forest headwater catchment calibrated against measured streamflow and transpiration from deciduous and coniferous stands. Simulations were corroborated by long-term (1965–2018) borehole measurements and historical drought reports. A regime shift from positive to negative catchment water balances likely occurred in the early part of this century. Since 2007, annual runoff: precipitation ratios have been below the long-term average. Annual average temperatures have increased, but there have been no notable long term trends in precipitation. Since 1980, there has been a pronounced April warming, likely leading to earlier leaf out and higher annual transpiration, making water unavailable for runoff generation and/or soil moisture recharge. Our results suggest a regime shift due to second order effects of climate change where increased transpiration associated with a longer growing season leads to a shift from light to water limitation in central European forests. This will require new approaches to managing forests where water limitation has previously not been a problem.


2020 ◽  
Author(s):  
Erin Alexander ◽  
◽  
Katelyn Weeks ◽  
Randall Debes ◽  
Lindsey Howe ◽  
...  

Geoderma ◽  
2000 ◽  
Vol 94 (1) ◽  
pp. 43-58 ◽  
Author(s):  
T Chevallier ◽  
M Voltz ◽  
E Blanchart ◽  
J.L Chotte ◽  
V Eschenbrenner ◽  
...  

2013 ◽  
Vol 15 (2) ◽  
pp. 101-110
Author(s):  
Joana Sender ◽  
Weronika Maślanko

ABSTRACT The Łęczna-Włodawa Plain, known also as the Łęczna-Wlodawa Lakeland, lies within the territory of the largest subregion of the Polesie region, covering over 1,300 km2. The main interest of the Łęczna-Włodawa Lakeland is that it is the oldest in the Central European Lowlands group of about 68 lakes. Among such a large number of lakes there exist all trophic types. However, since the late 1950’s, enormous dynamics of change associated with the disappearance of oligo- and mesotrophic lakes and their transformation into eutrophic, even hypertrophic, lakes have been observed. One of the biocenotic elements of the lakes, which are indicators of these changes, is aquatic plants. The aim of this study was to determine the macrophyte structure of Piaseczno Lake and changes of land use in its surroundings. Piaseczno Lake still represents very high natural values. A reduction in the number of macrophyte communities, which occurred especially in 2008, was a consequence of the fast-growing recreation infrastructure. From 1976 until 2010 an area of recreation infrastructure in the studied area increased more than 3.5 times, and in the built-up area more than five times, as well as a doubling of the total length of the roads. Meanwhile the surface area of wetlands and peatbogs significantly decreased - more than 11 times. Long-term changes in the structure of the macrophyte communities show that the number of communities has varied in each year, probably as a consequence of changes in landuse. Analysis showed changes to the surfaces inhabited by macrophytes, which have decreased significantly over only four years, by more than 25%. However, the proportion of rush communities has increased.


2000 ◽  
Vol 34 (8) ◽  
pp. 1521-1528 ◽  
Author(s):  
Trevor P. Rodgers-Gray ◽  
Susan Jobling ◽  
Steven Morris ◽  
Carole Kelly ◽  
Sonia Kirby ◽  
...  

2021 ◽  
Author(s):  
Alexander Moravek ◽  
Saumya Singh ◽  
Elizabeth Pattey ◽  
Amy Hdrina ◽  
Theodora Li ◽  
...  

<p>Emissions of ammonia (NH<sub>3</sub>) from agriculture have a significant impact on the environment. Its atmospheric transport and subsequent deposition has been shown to alter nutrient-poor ecosystems thereby reducing biodiversity. As the most abundant base in the atmosphere, NH<sub>3</sub> plays a key role in secondary aerosol formation impacting air quality and climate. Due to the lack of long term observations and challenges in performing NH<sub>3</sub> flux measurements, large uncertainties exist in both emission quantification from fertilized crop fields and in the bi-directional exchange of NH<sub>3</sub> with agroecosystems. We measured NH<sub>3</sub> fluxes above a corn field using the eddy covariance technique together with a quantum cascade laser spectroscopy analyzer over two consecutive growing seasons in 2017 and 2018. We found that after initial NH<sub>3</sub> emissions following fertilizer application, periods of both NH<sub>3</sub> emission and deposition with similar flux magnitudes prevailed throughout the growing seasons (ranging approximately between ±300 ng m<sup>-2</sup> s<sup>-1</sup>), highlighting the importance of the corn crop canopy for regulating the net NH<sub>3</sub> exchange. To evaluate the underlying processes of the NH<sub>3</sub> bi-directional exchange, a two-layer compensation point model was used. Based on the large range of environmental conditions encountered during the extensive flux measurements periods, the validity of different parameterizations could be assessed. In particular, processes regulating stomatal and non-stomatal flux pathways will be discussed.</p>


Author(s):  
Johann P. Arnason ◽  
Marek Hrubec

Problems of social revolutions and/or transformations belong to the classical agenda of social inquiry, as well as to the most prominent real and potential challenges encountered by contemporary societies. Among revolutionary events of the last decades, particular attention has been drawn to the changes that unfolded at the turn of the 1990s and brought the supposedly bipolar (in fact incipiently multipolar) world to an end. The downfall of East Central European Communist regimes in 1989 and of the Soviet Union in 1991 marked the beginning of a new era, originally characterised on the one hand by the relaxation of international tensions and on the other by the ascendancy of Western unilateralism. The twenty-fifth anniversary of the Soviet collapse prompts the authors of this book to reflect on revolutions and transformations, both from a long-term historical perspective and with regard to the post-Communist scene. The social changes unfolding in Eastern and Central Europe are not only epoch-making historical turns; their economic, social and political aspects, often confusing and unexpected, have also raised new questions and triggered debates about fundamental theoretical issues. Moreover, they have had a significant impact on developments elsewhere in the world, in both Western and developing countries.


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