scholarly journals Climate Change and Eutrophication: A Short Review

2018 ◽  
Vol 8 (6) ◽  
pp. 3668-3672
Author(s):  
M. Nazari Sharabian ◽  
S. Ahmad ◽  
M. Karakouzian
Keyword(s):  
Climate Change ◽  
Water Resources ◽  
Algal Blooms ◽  
Climatic Factors ◽  
Short Review ◽  
Human Beings ◽  
Nitrogen And Phosphorus ◽  
Factors Affecting ◽  
High Concentrations ◽  
Water Eutrophication

Water resources are vital not only for human beings but essentially all ecosystems. Human health is at risk if clean drinking water becomes contaminated. Water is also essential for agriculture, manufacturing, energy production and other diverse uses. Therefore, a changing climate and its potential effects put more pressure on water resources. Climate change may cause increased water demand as a result of rising temperatures and evaporation while decreasing water availability. On the other hand, extreme events as a result of climate change can increase surface runoff and flooding, deteriorating water quality as well. One effect is water eutrophication, which occurs when high concentrations of nutrients, such as nitrogen and phosphorus, are present in the water. Nutrients come from different sources including agriculture, wastewater, stormwater, and fossil fuel combustion. Algal blooms can cause many problems, such as deoxygenation and water toxicity, ultimately disrupting normal ecosystem functioning. In this paper, we investigate the potential impacts of climatic factors affecting water eutrophication, how these factors are projected to change in the future, and what their projected potential impacts will be.

scholarly journals Analysing the sensitivity of Hungarian landscapes based on climate change induced shallow groundwater fluctuation

2019 ◽  
Vol 68 (4) ◽  
pp. 355-372 ◽  
Author(s):  
Zoltán Zsolt Fehér ◽  
János Rakonczai
Keyword(s):  
Climate Change ◽  
Water Resources ◽  
Water Resource ◽  
Climatic Factors ◽  
Shallow Groundwater ◽  
Subsurface Water ◽  
Groundwater Fluctuation ◽  
Current Parameter ◽  
Local Water ◽  
The One

One of the undoubtedly recognizable consequences of the ongoing climate change in Hungary is the permanent change of groundwater depth, and consequently the sustainably reachable local water resources. These processes trigger remarkable changes in soil and vegetation. Thus, in research of sensitivity of any specific landscape to the varying climatic factors, monitoring and continuous evaluation of the water resources is inevitable. The presented spatiotemporal geostatistical cosimulation framework is capable to identify rearrangements of the subsurface water resources through water resource observations. Application of the Markov 2-type coregionalization model is based on the assumption, that presumably only slight changes have to be handled between two consecutive time instants, hence current parameter set can be estimated based on the spatial structures of prior and current dataset and previously identified parameters. Moreover, the algorithm is capable to take into consideration the significance of the geomorphologic settings on the subsurface water flow. Trends in water resource changes are appropriate indicators of certain areas climate sensitivity. The method is also suitable in determination of the main cause of the extraordinary groundwater discharges, like the one, observed from the beginning of the 1980’s in the Danube–Tisza Interfluve in Hungary.

Mitigating a global expansion of toxic cyanobacterial blooms: confounding effects and challenges posed by climate change

2020 ◽  
Vol 71 (5) ◽  
pp. 579 ◽  
Author(s):  
Hans W. Paerl ◽  
Karl. E. Havens ◽  
Nathan. S Hall ◽  
Timothy G. Otten ◽  
Mengyuan Zhu ◽  
...  
Keyword(s):  
Climate Change ◽  
Algal Blooms ◽  
Synergistic Effects ◽  
Cyanobacterial Blooms ◽  
Extreme Weather Events ◽  
Nutrient Load ◽  
Nitrogen And Phosphorus ◽  
Sediment Dredging ◽  
Fish Removal ◽  
Global Expansion

Managing and mitigating the global expansion of toxic cyanobacterial harmful algal blooms (CyanoHABs) is a major challenge facing researchers and water resource managers. Various approaches, including nutrient load reduction, artificial mixing and flushing, omnivorous fish removal, algaecide applications and sediment dredging, have been used to reduce bloom occurrences. However, managers now face the additional challenge of having to address the effects of climate change on watershed hydrological and nutrient load dynamics, water temperature, mixing regime and internal nutrient cycling. Rising temperatures and increasing frequencies and magnitudes of extreme weather events, including tropical cyclones, extratropical storms, floods and droughts, all promote CyanoHABs and affect the efficacy of ecosystem remediation measures. These climatic changes will likely require setting stricter nutrient (including both nitrogen and phosphorus) reduction targets for bloom control in affected waters. In addition, the efficacy of currently used methods to reduce CyanoHABs will need to be re-evaluated in light of the synergistic effects of climate change with nutrient enrichment.

scholarly journals The Runoff Evolution and the Differences Analysis of the Causes of Runoff Change in Different Regions: A Case of the Weihe River Basin, Northern China

2019 ◽  
Vol 11 (19) ◽  
pp. 5295 ◽  
Author(s):  
Shuoyang Li ◽  
Guiyu Yang ◽  
Hao Wang
Keyword(s):  
Climate Change ◽  
Water Resources ◽  
River Basin ◽  
Human Activity ◽  
Factors Affecting ◽  
Runoff Reduction ◽  
Runoff Change ◽  
Weihe River ◽  
Weihe River Basin ◽  
Impacts Of Human Activity

The runoff levels of the major hydrological stations in the Weihe river basin (WRB) have been found to present decreasing trends. However, the conspicuous spatial differences in the hydro-meteorological conditions have led to variations in the rainfall–runoff pattern in each of the sub-basin areas. The aims of this research study were to reveal the main factors contributing to the runoff changes in the different regions—and it has significance in the water resources rational allocation and protection in the different regions. Three statistical methods were used to analyze the law of precipitation and runoffs of five hydrological stations. The SWAT (Soil and Water Assessment Tool) model was used to reconstruct the runoff in the impact period. The effects of climate change and human activity on runoff were separated by comparing measured runoff and reconstructed runoff. The results show that the closer the proximity to the downstream hydrological station, the more the runoff decreased. In the tributaries and upstream hydrological stations (Zhuanhtou (ZT), Zhangjiashan (ZJS), and Linjiacun (LJC)), from 1970 to 2016, the dominant factor of the runoff reduction was determined to be climate change, and accounted for 148.2%, 98.9%, and 90.5%, respectively. In the hydrological stations of middle and lower reaches (Xianyang (XY) and Huaxian (HX)), the contributions of the climate change to the runoff reduction were 49.7% and 44.3%, respectively, and the impacts of human activity accounted for 50.3% and 55.7%. The impacts of human activity on the runoff reduction were slightly greater than that of the climate change. Due to the different leading factors affecting runoff change in the basin, in response to future climate change, for tributaries and upstream areas, land use should be rationally planned to achieve the optimal balance of water volume in each part of the basin, which is of great significance to the protection and utilization of water resources. As for the middle and downstream regions, reasonable planning should also be focused on the amount of water withdraw, water resource allocations, and water conservancy project construction. According to the factors affecting runoff, corresponding strategies are proposed for different regions, which have important research significance for the protection and sustainable development of watershed water resources.

scholarly journals Influences of Shifted Vegetation Phenology on Runoff Across a Hydroclimatic Gradient

2022 ◽  
Vol 12 ◽  
Author(s):  
Shouzhi Chen ◽  
Yongshuo H. Fu ◽  
Xiaojun Geng ◽  
Zengchao Hao ◽  
Jing Tang ◽  
...  
Keyword(s):  
Climate Change ◽  
Climatic Factors ◽  
Remote Sensing Data ◽  
River Basins ◽  
Gray Relational Analysis ◽  
Vegetation Phenology ◽  
Spring Phenology ◽  
Factors Affecting ◽  
Growing Season Length ◽  
Humid Region

Climate warming has changed vegetation phenology, and the phenology-associated impacts on terrestrial water fluxes remain largely unquantified. The impacts are linked to plant adjustments and responses to climate change and can be different in different hydroclimatic regions. Based on remote sensing data and observed river runoff of hydrological station from six river basins across a hydroclimatic gradient from northeast to southwest in China, the relative contributions of the vegetation (including spring and autumn phenology, growing season length (GSL), and gross primary productivity) and climatic factors affecting the river runoffs over 1982–2015 were investigated by applying gray relational analysis (GRA). We found that the average GSLs in humid regions (190–241 days) were longer than that in semi-humid regions (186–192 days), and the average GSLs were consistently extended by 4.8–13.9 days in 1982–2015 period in six river basins. The extensions were mainly linked to the delayed autumn phenology in the humid regions and to advanced spring phenology in the semi-humid regions. Across all river basins, the GRA results showed that precipitation (r = 0.74) and soil moisture (r = 0.73) determine the river runoffs, and the vegetation factors (VFs) especially the vegetation phenology also affected the river runoffs (spring phenology: r = 0.66; GSL: r = 0.61; autumn phenology: r = 0.59), even larger than the contribution from temperature (r = 0.57), but its relative importance is climatic region-dependent. Interestingly, the spring phenology is the main VF in the humid region for runoffs reduction, while both spring and autumn growth phenology are the main VFs in the semi-humid region, because large autumn phenology delay and less water supply capacity in spring amplify the effect of advanced spring phenology. This article reveals diverse linkages between climatic and VFs, and runoff in different hydroclimatic regions, and provides insights that vegetation phenology influences the ecohydrology process largely depending on the local hydroclimatic conditions, which improve our understanding of terrestrial hydrological responses to climate change.

scholarly journals Impact of climate changes on water resources of Kuialnyk Liman catchment in scenario climate conditions

2017 ◽  
pp. 189-195
Author(s):  
N.S. Loboda ◽  
Y.V. Bozhok
Keyword(s):  
Climate Change ◽  
Water Resources ◽  
Regional Climate Model ◽  
Climate Model ◽  
Climatic Factors ◽  
Global Climate ◽  
Regional Climate ◽  
Climate Change Scenarios ◽  
Climate Conditions ◽  
Surrounding Areas

The actuality of research is conditioned by necessity of water regime determination under climate change for substantiate management its water resources in future. The purpose of investigation is evaluation of changes in water resources of Kuyalnyk Liman catchment under climate change. The main method of research is model "climate- runoff ", developed at the Odessa State Environmental University. Database of global climate change scenarios A1B (realized in regional climate model REMO) and A2 (developed under the regional climate model RCA) was used. The analysis of fluctuation regularity of climatic factors of the flow formation on the Kuyalnyk  Liman catchment and surrounding areas according to selected scenarios using  difference-integral curves are done. Changes in precipitation and the maximum possible evaporation for the 30-year intervals up to the year 2100 (scenario A1D) or up to the year 2050 (scenario A2) are analyzed. The main tendencies in water resources of Kuyalnyk Liman using the model "climate- runoff" in the future are established. It is shown that according to the scenario A1B by the middle of XXI century possible reduction of water resources in the Kuyalnyk Liman catchment is 40%. According to the scenario A2 water resources in northern part of the basin can grow on average by 20-30%, and in the southern part runoff can be reduced on average by 10%.

scholarly journals Analysis of runoff characteristics and contribution rate in Xiying River Basin in the Eastern Qilian Mountains

2019 ◽  
Vol 136 ◽  
pp. 04014
Author(s):  
Lei Feng ◽  
Dong Yang ◽  
Yueyue Huang
Keyword(s):  
Climate Change ◽  
Water Resources ◽  
Climatic Factors ◽  
Potential Evapotranspiration ◽  
Qilian Mountains ◽  
Snow Melt ◽  
Contribution Rate ◽  
Natural Ecosystems ◽  
Melt Water ◽  
The Impact

The impact of climate change on the basin is extensive and long-lasting, which will have a profound impact on the natural ecosystems, water resources, agriculture, and human production and life throughout the basin. An in-depth understanding of the impacts of climate change on watersheds and quantitative assessments will help to scientifically plan and manage water resources and protect the integrity of natural ecosystems. In this paper, temperature, precipitation and potential evapotranspiration data were used to analyze the response of Xiying River runoff to climatic factors in the Qilian Mountains by sliding correlation and wavelet analysis. M-K test and cumulative anomaly (CA) were used to analyze the climatic factors and runoff in the basin and use the pettitt method to test. Finally, the cumulative rate slope change rate comparison method was used to analyze the change of precipitation, potential evapotranspiration and snow-melt water contribution to runoff in this area. The results showed that temperature, precipitation and potential evapotranspiration had obvious mutations from 1961 to 2012 in this region. Compared with temperature and potential evapotranspiration, the precipitation showed greater impact on runoff. In addition, the contribution rate of ice and snow melt water to runoff was relatively larger in 1990 - 2002 compared to 1961-1989, followed by precipitation and evapotranspiration; the increase of the precipitation contribution rate became the main factor to runoff, followed by ice and snow melting and evapotranspiration compared to 1990-2002 in 2003-2017.

Religion in the Age of the Anthropocene

2019 ◽  
Author(s):  
Arianne F. Conty
Keyword(s):  
Social Sciences ◽  
Climate Change ◽  
Natural Sciences ◽  
Human Beings ◽  
Risks And Benefits ◽  
Human Exceptionalism ◽  
The Earth ◽  
Contemporary Christian ◽  
Genesis 1 ◽  
Forms Of Life

Though responses to the Anthropocene have largely come from the natural and social sciences, religious responses to the Anthropocene have also been gaining momentum and many scholars have been calling for a religious response to complement scientific responses to climate change. Yet because Genesis 1:28 does indeed tell human beings to ‘subdue the earth’ monotheistic religions have often been understood as complicit in the human exceptionalism that is thought to have created the conditions for the Anthropocene. In distinction to such Biblical traditions, indigenous animistic cultures have typically respected all forms of life as ‘persons’ and such traditions have thus become a source of inspiration for ecological movements. After discussing contemporary Christian efforts to integrate the natural sciences and the environment into their responses to the Anthropocene, this article will turn to animism and seek to evaluate the risks and benefits that could ensue from a postmodern form of animism that could provide a necessary postsecular response to the Anthropocene.

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