scholarly journals Land‐use dominates climate controls on nitrogen and phosphorus export from managed and natural Nordic headwater catchments

2020 ◽  
Vol 34 (25) ◽  
pp. 4831-4850
Author(s):  
Heleen A. Wit ◽  
Ahti Lepistö ◽  
Hannu Marttila ◽  
Hannah Wenng ◽  
Marianne Bechmann ◽  
...  
2013 ◽  
Vol 28 (8) ◽  
pp. 3201-3216 ◽  
Author(s):  
Samson G. Mengistu ◽  
Irena F. Creed ◽  
Kara L. Webster ◽  
Eric Enanga ◽  
Frederick D. Beall

2018 ◽  
Vol 19 (1) ◽  
pp. 275-285 ◽  
Author(s):  
Luying Wang ◽  
Xiaofei Yu ◽  
Zhenshan Xue ◽  
Lili Huo ◽  
Ming Jiang ◽  
...  

2015 ◽  
Vol 44 (5) ◽  
pp. 1589-1604 ◽  
Author(s):  
M. D. Sunohara ◽  
N. Gottschall ◽  
G. Wilkes ◽  
E. Craiovan ◽  
E. Topp ◽  
...  

2020 ◽  
Author(s):  
Andrea Critto ◽  
Hung Vuong Pham ◽  
Anna Sperotto ◽  
Silvia Torresan ◽  
Elisa Furlan ◽  
...  

<p>Freshwater ecosystems can be negatively affected by climate change and human interventions through the alteration of water supply and demand. There is an urgent need to protect the ecosystems, and the services they provide, to maintain their essential contribution to human wellbeing and economic prosperity, especially in a rapid and unpredictable global change context. In this work, we developed an integrated approach, coupling the outputs of ecosystem services (InVEST), climate (COSMO-CLM) and land use (LUISA) change models utilizing Bayesian Networks (BNs), to map freshwater-related Ecosystem Services (ESs), namely, water yield, nitrogen and phosphorus retention, and to assess their changes until 2050 under different management scenarios. First, InVEST was calibrated and validated with climate and land-use data to map and quantify ESs. Second, outputs of the ES model were integrated into the BN and the changes induced by different learning techniques and input settings were investigated. Finally, thousands of different scenarios were simulated testing multiple input variables configurations, thus allowing to describe the uncertainty of climate conditions, land-use change and water demand. Two types of inferences were conducted, namely, diagnostic and prognostic inference. The former permitted to find the best combination of the key drivers (i.e.  precipitation, land-use, and water demand) so that ESs are maximized while the latter concentrated on the quantification of ESs under different scenarios. This approach was applied and validated in the Taro River basin in Italy. The results show that the values of all the three types of ESs would decline in the medium-term period under most scenarios. Moreover, there would be a limit of space to improve those values, especially for nutrient retention services. The obtained results provide valuable support to identify and prioritize the best management practices for sustainable water use, balancing the tradeoffs among services. This analysis allows decision-makers to pick up one scenario with a specific configuration of land-use and water demand to optimize relevant ESs within their basin. Finally, these decisions are transformed into a “decision space” where the values of selected services are plotted in the space of ES to represent the gain/loss of each decision.</p>


2020 ◽  
Author(s):  
Shovon Barua ◽  
Ian Cartwright ◽  
Edoardo Daly ◽  
Uwe Morgenstern

<p>Intermittent headwater catchments constitute a significant proportion of many stream networks. In semi-arid climates, intermittent headwater streams flow only following periods of sustained rainfall. There is commonly a rapid response of streamflow to rainfall; however, whether this is the input of recent rainfall or displacement of water stored in the catchments for several years is not well known. Understanding the sources and transit times of water that contribute to streamflow is important for the maintenance of stream health and predicting the response of land-use changes.</p><p>The study focuses on two intermittent streams from two contrasting land-use (pasture and forest) in southeast Australia. The native eucalyptus forests in this region were originally cleared for grazing following European settlement <sup>~</sup>180 years ago and then partially replaced by plantation in the last <sup>~</sup>15 years. Stream water and groundwater from the riparian zone adjacent to the streams were sampled between May and October 2018.</p><p>The stream water has <sup>3</sup>H activities of 1.30 to 3.17 TU in the pasture and 1.84 to 3.99 TU in the forest, with higher activities recorded during the higher winter flows. Groundwater from the riparian zone has <sup>3</sup>H activities of 0.16 to 0.79 TU in the pasture and 2.01 to 4.10 TU in the forest. Aside from one riparian zone groundwater sample, all <sup>3</sup>H activities of groundwater in the riparian zone are lower than those of recent local rainfall (<sup>~</sup>2.79 TU). The single high <sup>3</sup>H activity in riparian zone possibly reflects recharge by winter rainfall with higher <sup>3</sup>H activities.</p><p>The mean transit times (MTTs) of water were estimated using a range of tracer lumped parameter models. The riparian zone groundwater has greater MTTs of hundreds of years in the pasture and up to 9 years in the forest. At high streamflow, the stream water has MTTs of <6 years in the pasture and the forest. The MTTs of stream water at low streamflow vary from 15 to 42 years in the pasture and from 3 to 16 years in the forest. The long MTTs of water from streams indicate that the source water is not just recent rainfall, rather water stored in the riparian zone is mobilised at the commencement of flow and recent rainfall makes a larger contribution at higher flows. The observation is consistent with the major ion geochemistry of the stream water, which most closely represents that of the riparian zone groundwater. The differences in MTTs of stream water between two contrasting land-use imply that the streamflow has been being most likely impacted by land-use changes. Thus, it is necessary to improve the strategies for catchment management to protect stream health from land-use practices.</p>


Plant Ecology ◽  
2010 ◽  
Vol 212 (5) ◽  
pp. 901-909 ◽  
Author(s):  
Lander Baeten ◽  
Gorik Verstraeten ◽  
Pieter De Frenne ◽  
Margot Vanhellemont ◽  
Karen Wuyts ◽  
...  

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