A catchment-scale carbon and greenhouse gas budget of a subarctic landscape

2007 ◽  
Vol 365 (1856) ◽  
pp. 1643-1656 ◽  
Author(s):  
T.R Christensen ◽  
T Johansson ◽  
M Olsrud ◽  
L Ström ◽  
A Lindroth ◽  
...  
Keyword(s):  
Greenhouse Gas ◽  
Radiative Forcing ◽  
Environmental Changes ◽  
Catchment Scale ◽  
Run Off ◽  
Sink Capacity ◽  
Catchment Budget ◽  
Annual Carbon ◽  
Average Current ◽  
The Individual

This is the first attempt to budget average current annual carbon (C) and associated greenhouse gas (GHG) exchanges and transfers in a subarctic landscape, the Lake Torneträsk catchment in northern Sweden. This is a heterogeneous area consisting of almost 4000 km 2 of mixed heath, birch and pine forest, and mires, lakes and alpine ecosystems. The magnitudes of atmospheric exchange of carbon in the form of the GHGs, CO 2 and CH 4 in these various ecosystems differ significantly, ranging from little or no flux in barren ecosystems over a small CO 2 sink function and low rates of CH 4 exchange in the heaths to significant CO 2 uptake in the forests and also large emissions of CH 4 from the mires and small lakes. The overall catchment budget, given the size distribution of the individual ecosystem types and a first approximation of run-off as dissolved organic carbon, reveals a landscape currently with a significant sink capacity for atmospheric CO 2 . This sink capacity is, however, extremely sensitive to environmental changes, particularly those that affect the birch forest ecosystem. Climatic drying or wetting and episodic events such as insect outbreaks may cause significant changes in the sink function. Changes in the sources of CH 4 through increased permafrost melting may also easily change the sign of the current radiative forcing, due to the stronger impact per gram of CH 4 relative to CO 2 . Hence, to access impacts on climate, the atmospheric C balance alone has to be weighed in a radiative forcing perspective. When considering the emissions of CH 4 from the mires and lakes as CO 2 equivalents, the Torneträsk catchment is currently a smaller sink of radiative forcing, but it can still be estimated as representing the equivalent of approximately 14 000 average Swedish inhabitants' emissions of CO 2 . This can be compared with the carbon emissions of less than 200 people who live permanently in the catchment, although this comparison disregards substantial emissions from the non-Swedish tourism and transportation activities.

scholarly journals Impacts des changements climatique et environnemental sur la réponse hydrologique du bassin du Nakanbé à Wayen (Burkina Faso) à travers le cadre de budyko

2021 ◽  
Vol 384 ◽  
pp. 269-273
Author(s):  
Yetchékpo Patrick Gbohoui ◽  
Jean-Emmanuel Paturel ◽  
Tazen Fowe ◽  
Harouna Karambiri ◽  
Hamma Yacouba
Keyword(s):  
Climate Change ◽  
Environmental Changes ◽  
Potential Evapotranspiration ◽  
Statistical Tests ◽  
Annual Runoff ◽  
P Value ◽  
Climatic Data ◽  
Catchment Scale ◽  
Pettitt Test ◽  
The Individual

Abstract. Les changements climatique et environnemental ont entraîné l'augmentation exacerbée des coefficients d'écoulement dans certains hydrosystèmes du Sahel ouest africain. Ce «paradoxe hydrologique sahélien» a fait l'objet de plusieurs études, mais très peu d'entre elles ont abordé les contributions de chacun des changements climatique et environnemental. L'objectif de cette étude est de quantifier les contributions de chacun des facteurs (climat et environnement) au changement des écoulements dans la partie sahélienne du bassin du Nakanbé sur la période 1965–1994. Les tests statistiques de stationnarité ont permis de découper la période d'étude en sous-périodes de base et d'impact. La quantification des impacts a été effectuée à travers l'application des techniques d'élasticité et de décomposition aux modèles Budyko de Fu et de Choudhury. L'analyse des chroniques de données hydro-climatiques du bassin a confirmé le paradoxe hydrologique avec une rupture dans les écoulements en 1977 (test de Pettitt, p value = 0,021). Ainsi, la période 1978–1994 comparativement à 1965–1977 a été caractérisée par une diminution des précipitations de 8,2 %, une augmentation de l'évapotranspiration potentielle de 1,3 % et une augmentation des écoulements de 91,5 %. Il ressort de cette étude que les contributions à l'augmentation des écoulements de 91,5 % ont été de -29±2 % pour le changement climatique, +90±1 % pour la dégradation environnementale et +33 % pour les interactions couplées climat-environnement. Ces résultats montrent que l'impact de l'environnement est plus prépondérant et représente environ 3 fois celui du climat en intensité. L'adoption de meilleures pratiques de gestion de la dynamique environnementale pourrait donc permettre de réguler les changements dans les écoulements du bassin. Abstract. Climate and environmental changes have caused the increasing runoff coefficients of some sahelian catchments in West Africa. Many previous studies have focused on this “sahelian hydrological paradox”, but few have addressed the individual contribution of climate and the environment. This study aims to quantify the contributions of each factor (climate and environment) to the change of runoff in the sahelian part of the Nakanbé catchment over the period : 1965–1994. Based on time-series stationarity statistical tests, the study period was divided into baseline and impacted periods. The quantification of impacts was carried out by applying elasticity and decomposition techniques to the Budyko type models of Fu and Choudhury. Statistical analysis of the annual hydro-climatic data detected 1977 as the year of break in the runoff (Pettitt test, p value = 0.021) and confirmed the sahelian hydrological paradox. Thus, the period 1978–1994 compared to 1965–1977 was characterized by a decrease of 8.2 % in precipitation while increases of 1.3 % and 91.5 % have been observed respectively for potential evapotranspiration and annual runoff. The results indicated that the contributions to the runoff increase of 91.5 % were -29±2 % for climate change, +90±1 % for environmental degradation and +33 % for interactions. It appears that, environmental change is the main cause of the increase in the runoff coefficient in the sahelian catchment of Nakanbé and the intensity of its impact is approximately 3 times more than the one induced by climate change. Therefore, good management of environmental dynamics at the catchment scale could help to regulate runoff changes.

Past testate amoeba communities in landslide mountain fens (Polish Carpathians): The relationship between shell types and sediment

The Holocene ◽  
2021 ◽  
pp. 095968362199464
Author(s):  
Katarzyna Marcisz ◽  
Krzysztof Buczek ◽  
Mariusz Gałka ◽  
Włodzimierz Margielewski ◽  
Matthieu Mulot ◽  
...  
Keyword(s):  
Environmental Changes ◽  
Testate Amoebae ◽  
Mineral Matter ◽  
Testate Amoeba ◽  
Run Off ◽  
Number Of Factors ◽  
Depth To Water Table ◽  
Polish Carpathians ◽  
The Relationship

Landslide mountain fens formed in landslide depressions are dynamic environments as their development is disturbed by a number of factors, for example, landslides, slopewash, and surface run-off. These processes lead to the accumulation of mineral material and wood in peat. Disturbed peatlands are interesting archives of past environmental changes, but they may be challenging for providing biotic proxy-based quantitative reconstructions. Here we investigate long-term changes in testate amoeba communities from two landslide mountain fens – so far an overlooked habitat for testate amoeba investigations. Our results show that abundances of testate amoebae are extremely low in this type of peatlands, therefore not suitable for providing quantitative depth-to-water table reconstructions. However, frequent shifts of dominant testate amoeba species reflect dynamic lithological situation of the studied fens. We observed that high and stable mineral matter input into the peatlands was associated with high abundances of species producing agglutinated (xenosomic) as well as idiosomic shells which prevailed in the testate amoeba communities in both analyzed profiles. This is the first study that explores testate amoebae of landslide mountain fens in such detail, providing novel information about microbial communities of these ecosystems.

scholarly journals Impact of Cycle Time and Payload of an Industrial Robot on Resource Efficiency

Robotics ◽  
2021 ◽  
Vol 10 (1) ◽  
pp. 33
Author(s):  
Florian Stuhlenmiller ◽  
Steffi Weyand ◽  
Jens Jungblut ◽  
Liselotte Schebek ◽  
Debora Clever ◽  
...  
Keyword(s):  
Life Cycle Assessment ◽  
Life Cycle ◽  
Energy Consumption ◽  
Greenhouse Gas Emissions ◽  
Greenhouse Gas ◽  
Resource Efficiency ◽  
Life Cycle Costs ◽  
Gas Emissions ◽  
Cycle Times ◽  
The Individual

Modern industry benefits from the automation capabilities and flexibility of robots. Consequently, the performance depends on the individual task, robot and trajectory, while application periods of several years lead to a significant impact of the use phase on the resource efficiency. In this work, simulation models predicting a robot’s energy consumption are extended by an estimation of the reliability, enabling the consideration of maintenance to enhance the assessment of the application’s life cycle costs. Furthermore, a life cycle assessment yields the greenhouse gas emissions for the individual application. Potential benefits of the combination of motion simulation and cost analysis are highlighted by the application to an exemplary system. For the selected application, the consumed energy has a distinct impact on greenhouse gas emissions, while acquisition costs govern life cycle costs. Low cycle times result in reduced costs per workpiece, however, for short cycle times and higher payloads, the probability of required spare parts distinctly increases for two critical robotic joints. Hence, the analysis of energy consumption and reliability, in combination with maintenance, life cycle costing and life cycle assessment, can provide additional information to improve the resource efficiency.

scholarly journals When physical activity meets the physical environment: precision health insights from the intersection

2021 ◽  
Vol 26 (1) ◽  
Author(s):  
Luisa V. Giles ◽  
Michael S. Koehle ◽  
Brian E. Saelens ◽  
Hind Sbihi ◽  
Chris Carlsten
Keyword(s):  
Physical Activity ◽  
Physical Environment ◽  
Environmental Changes ◽  
Main Body ◽  
Or Groups ◽  
Optimizing Design ◽  
Physical Activity Recommendations ◽  
The Individual ◽  
Precision Health ◽  
Activity Recommendations

Abstract Background The physical environment can facilitate or hinder physical activity. A challenge in promoting physical activity is ensuring that the physical environment is supportive and that these supports are appropriately tailored to the individual or group in question. Ideally, aspects of the environment that impact physical activity would be enhanced, but environmental changes take time, and identifying ways to provide more precision to physical activity recommendations might be helpful for specific individuals or groups. Therefore, moving beyond a “one size fits all” to a precision-based approach is critical. Main body To this end, we considered 4 critical aspects of the physical environment that influence physical activity (walkability, green space, traffic-related air pollution, and heat) and how these aspects could enhance our ability to precisely guide physical activity. Strategies to increase physical activity could include optimizing design of the built environment or mitigating of some of the environmental impediments to activity through personalized or population-wide interventions. Conclusions Although at present non-personalized approaches may be more widespread than those tailored to one person’s physical environment, targeting intrinsic personal elements (e.g., medical conditions, sex, age, socioeconomic status) has interesting potential to enhance the likelihood and ability of individuals to participate in physical activity.

scholarly journals Revisiting the Agung 1963 volcanic forcing – impact of one or two eruptions

2019 ◽  
Author(s):  
Ulrike Niemeier ◽  
Claudia Timmreck ◽  
Kirstin Krüger
Keyword(s):  
Radiative Forcing ◽  
Injection Rate ◽  
Data Sets ◽  
Meridional Transport ◽  
Emission Data ◽  
Volcanic Clouds ◽  
Different Seasons ◽  
Future Emission ◽  
Volcanic Emission ◽  
The Individual

Abstract. In 1963 a series of eruptions of Mt. Agung, Indonesia, resulted in the 3rd largest eruption of the 20th century and claimed about 1900 lives. Two eruptions of this series injected SO2 into the stratosphere, a requirement to get a long lasting stratospheric sulfate layer. The first eruption on March 17th injected 4.7 Tg SO2 into the stratosphere, the second eruption 2.3 Tg SO2 on May, 16th. In recent volcanic emission data sets these eruption phases are merged together to one large eruption phase for Mt. Agung in March 1963 with an injection rate of 7 Tg SO2. The injected sulfur forms a sulfate layer in the stratosphere. The evolution of sulfur is non-linear and depends on the injection rate and aerosol background conditions. We performed ensembles of two model experiments, one with a single and a second one with two eruptions. The two smaller eruptions result in a lower burden, smaller particles and 0.1 to 0.3 Wm−2 (10–20 %) lower radiative forcing in monthly mean global average compared to the individual eruption experiment. The differences are the consequence of slightly stronger meridional transport due to different seasons of the eruptions, lower injection height of the second eruption and the resulting different aerosol evolution. The differences between the two experiments are significant but smaller than the variance of the individual ensemble means. Overall, the evolution of the volcanic clouds is different in case of two eruptions than with a single eruption only. We conclude that there is no justification to use one eruption only and both climatic eruptions should be taken into account in future emission datasets.

scholarly journals The Protective Role of Butyrate against Obesity and Obesity-Related Diseases

Molecules ◽  
2021 ◽  
Vol 26 (3) ◽  
pp. 682
Author(s):  
Serena Coppola ◽  
Carmen Avagliano ◽  
Antonio Calignano ◽  
Roberto Berni Canani
Keyword(s):  
Metabolic Diseases ◽  
Environmental Changes ◽  
Short Chain Fatty Acids ◽  
Protective Role ◽  
Health Concern ◽  
Predisposing Factor ◽  
Alcoholic Fatty Liver ◽  
Beneficial Effects ◽  
The Individual

Worldwide obesity is a public health concern that has reached pandemic levels. Obesity is the major predisposing factor to comorbidities, including type 2 diabetes, cardiovascular diseases, dyslipidemia, and non-alcoholic fatty liver disease. The common forms of obesity are multifactorial and derive from a complex interplay of environmental changes and the individual genetic predisposition. Increasing evidence suggest a pivotal role played by alterations of gut microbiota (GM) that could represent the causative link between environmental factors and onset of obesity. The beneficial effects of GM are mainly mediated by the secretion of various metabolites. Short-chain fatty acids (SCFAs) acetate, propionate and butyrate are small organic metabolites produced by fermentation of dietary fibers and resistant starch with vast beneficial effects in energy metabolism, intestinal homeostasis and immune responses regulation. An aberrant production of SCFAs has emerged in obesity and metabolic diseases. Among SCFAs, butyrate emerged because it might have a potential in alleviating obesity and related comorbidities. Here we reviewed the preclinical and clinical data that contribute to explain the role of butyrate in this context, highlighting its crucial contribute in the diet-GM-host health axis.

Greenhouse gas budget of an extensively managed grassland on drained peat soil in the Irish Midlands

2021 ◽  
Author(s):  
Marine Valmier ◽  
Matthew Saunders ◽  
Gary Lanigan
Keyword(s):  
Carbon Source ◽  
Greenhouse Gas ◽  
Ghg Emissions ◽  
Organic Soils ◽  
Climate Mitigation ◽  
Sink Strength ◽  
Management Options ◽  
Peat Soils ◽  
Sequestration Potential ◽  
Sink Capacity

<p>Grassland-based agriculture in Ireland contributes over one third of national greenhouse gas (GHG) emissions, and the LULUCF sector is a net GHG source primarily due to the ongoing drainage of peat soils. Rewetting of peat-based organic soils is now recognised as an attractive climate mitigation strategy, but reducing emissions and restoring the carbon sequestration potential is challenging, and is not always feasible notably due to agricultural demands. Nonetheless, reducing carbon losses from drained organic soils has been identified as a key action for Ireland to reach its climate targets, and carbon storage associated with improved grassland management practices can provide a suitable strategy to offset GHG emissions without compromising productivity. However, research is still needed to assess the best practices and management options for optimum environmental and production outcomes. While grasslands have been widely studied internationally, data on organic soils under this land use are still scarce. In Ireland, despite their spatial extent and relevance to the national emission inventories and mitigation strategies, only two studies on GHG emissions from grasslands on peat soils have been published.</p><p>Here we present results from a grassland on a drained organic soil that is extensively managed for silage production in the Irish midlands. Continuous monitoring of Net Ecosystem Exchange (NEE) of carbon dioxide (CO<sub>2</sub>) using eddy covariance techniques, and weekly static chamber measurements to assess soil derived emissions of methane (CH<sub>4</sub>) and nitrous oxide (N<sub>2</sub>O) started in 2020. The seasonal CO<sub>2</sub> fluxes observed were greatly dependent on weather conditions and management events. The grassland shifted from a carbon source at the beginning of the year to a sink during the growing season, with carbon uptakes in April and May ranging from 15 to 40 µmol CO<sub>2</sub> m<sup>-2</sup> s<sup>-1</sup> and releases in the order of 5 µmol CO<sub>2</sub> m<sup>-2</sup> s<sup>-1</sup>. Following the first harvest event in early June, approximately 2.5 t C ha<sup>-1</sup> was exported, and the sink capacity took around one month to recover, with an average NEE of 10 µmol CO<sub>2</sub> m<sup>-2</sup> s<sup>-1</sup> during that period. Carbon uptake then reached a maximum of 25 µmol CO<sub>2</sub> m<sup>-2</sup> s<sup>-1</sup> in August. After the second cut in mid-September, which corresponded to an export of 2.25 t.ha<sup>-1</sup> of carbon, the grassland acted once again as a strong carbon source, losing almost 30 g C m<sup>-2</sup> in a month, before stabilising and behaving as an overall small source during the winter period.</p><p>In summary, this grassland demonstrated high rates of carbon assimilation and productivity that translate in a strong carbon sink capacity highly dependent on the management. The biomass harvest is a major component of the annual budget that has the potential to shift the system to a net carbon source. Moreover, while initial measurements of CH<sub>4</sub> and N<sub>2</sub>O fluxes appeared to be negligible, some management events were not assessed due to national COVID 19 restrictions on movement, which might have impacted the sink strength of the site studied.</p>

scholarly journals Historical greenhouse gas concentrations

2016 ◽  
Author(s):  
Malte Meinshausen ◽  
Elisabeth Vogel ◽  
Alexander Nauels ◽  
Katja Lorbacher ◽  
Nicolai Meinshausen ◽  
...  
Keyword(s):  
Climate Change ◽  
Greenhouse Gas ◽  
Radiative Forcing ◽  
Sulfur Hexafluoride ◽  
Climate Model ◽  
Future Climate Change ◽  
Large Set ◽  
Mixing Ratios ◽  
Surface Mixing ◽  
Cooling Effects

Abstract. Atmospheric greenhouse gas concentrations are at unprecedented, record-high levels compared to pre-industrial reconstructions over the last 800,000 years. Those elevated greenhouse gas concentrations warm the planet and together with net cooling effects by aerosols, they are the reason of observed climate change over the past 150 years. An accurate representation of those concentrations is hence important to understand and model recent and future climate change. So far, community efforts to create composite datasets with seasonal and latitudinal information have focused on marine boundary layer conditions and recent trends since 1980s. Here, we provide consolidated data sets of historical atmospheric (volume) mixing ratios of 43 greenhouse gases specifically for the purpose of climate model runs. The presented datasets are based on AGAGE and NOAA networks and a large set of literature studies. In contrast to previous intercomparisons, the new datasets are latitudinally resolved, and include seasonality over the period between year 0 to 2014. We assimilate data for CO2, methane (CH4) and nitrous oxide (N2O), 5 chlorofluorocarbons (CFCs), 3 hydrochlorofluorocarbons (HCFCs), 16 hydrofluorocarbons (HFCs), 3 halons, methyl bromide (CH3Br), 3 perfluorocarbons (PFCs), sulfur hexafluoride (SF6), nitrogen triflouride (NF3) and sulfuryl fluoride (SO2F2). We estimate 1850 annual and global mean surface mixing ratios of CO2 at 284.3 ppmv, CH4 at 808.2 ppbv and N2O at 273.0 ppbv and quantify the seasonal and hemispheric gradients of surface mixing ratios. Compared to earlier intercomparisons, the stronger implied radiative forcing in the northern hemisphere winter (due to the latitudinal gradient and seasonality) may help to improve the skill of climate models to reproduce past climate and thereby reduce uncertainty in future projections.

scholarly journals Chemical and climatic drivers of radiative forcing due to changes in stratospheric and tropospheric ozone over the 21<sup>st</sup> century

2017 ◽  
Author(s):  
Antara Banerjee ◽  
Amanda C. Maycock ◽  
John A. Pyle
Keyword(s):  
Greenhouse Gas ◽  
Tropospheric Ozone ◽  
Radiative Forcing ◽  
Climate Model ◽  
Stratospheric Ozone ◽  
Radiative Forcings ◽  
Climatic Drivers ◽  
Ozone Precursor ◽  
Ozone Depleting Substances ◽  
Projected Changes

Abstract. The ozone radiative forcings (RFs) resulting from projected changes in climate, ozone-depleting substances (ODSs), non-methane ozone precursor emissions and methane between the years 2000 and 2100 are calculated using simulations from the UM-UKCA chemistry-climate model. Projected measures to improve air-quality through reductions in tropospheric ozone precursor emissions present a co-benefit for climate, with a net global mean ozone RF of −0.09 Wm−2. This is opposed by a positive ozone RF of 0.07 Wm−2 due to future decreases in ODSs, which is mainly driven by an increase in tropospheric ozone through stratosphere-to-troposphere exchange. An increase in methane abundance by more than a factor of two (as projected by the RCP8.5 scenario) is found to drive an ozone RF of 0.19 Wm−2, which would greatly outweigh the climate benefits of tropospheric non-methane ozone precursor reductions. A third of the ozone RF due to the projected increase in methane results from increases in stratospheric ozone. The sign of the ozone RF due to future changes in climate (including the radiative effects of greenhouse gas concentrations, sea surface temperatures and sea ice changes) is shown to be dependent on the greenhouse gas emissions pathway, with a positive RF (0.06 Wm−2) for RCP4.5 and a negative RF (−0.07 Wm−2) for the RCP8.5 scenario. This dependence arises from differences in the contribution to RF from stratospheric ozone changes.

scholarly journals Synthesizing greenhouse gas fluxes across nine European peatlands and shrublands – responses to climatic and environmental changes

2012 ◽  
Vol 9 (3) ◽  
pp. 3693-3738 ◽  
Author(s):  
M. S. Carter ◽  
K. S. Larsen ◽  
B. Emmett ◽  
M. Estiarte ◽  
C. Field ◽  
...  
Keyword(s):  
Global Warming ◽  
Greenhouse Gas ◽  
Air Temperature ◽  
Environmental Changes ◽  
Negative Relationship ◽  
Co2 Efflux ◽  
Soil Co2 ◽  
Prolonged Drought ◽  
Mean Annual Air Temperature

Abstract. In this study, we compare annual fluxes of methane (CH4), nitrous oxide (N2O) and soil respiratory carbon dioxide (CO2) measured at nine European peatlands (n = 4) and shrublands (n = 5). The sites range from northern Sweden to Spain, covering a span in mean annual air temperature from 0 to 16 °C, and in annual precipitation from 300 to 1300 mm yr−1. The effects of climate change, including temperature increase and prolonged drought, were tested at five shrubland sites. At one peatland site, the long-term (>30 yr) effect of drainage was assessed, while increased nitrogen deposition was investigated at three peatland sites. The shrublands were generally sinks for atmospheric CH4 whereas the peatlands were CH4 sources, with fluxes ranging from −519 to +6890 mg CH4-C m−2 yr−1 across the studied ecosystems. At the peatland sites, annual CH4 emission increased with mean annual air temperature, while a negative relationship was found between net CH4 uptake and the soil carbon stock at the shrubland sites. Annual N2O fluxes were generally small ranging from –14 to 42 mg N2O-N m−2 yr−1. Highest N2O emission occurred at the sites that had highest concentration of nitrate (NO3−) in soil water. Furthermore, experimentally increased NO3− deposition led to increased N2O efflux, whereas prolonged drought and long-term drainage reduced the N2O efflux. Soil CO2 emissions in control plots ranged from 310 to 732 g CO2-C m−2 yr−1. Drought and long-term drainage generally reduced the soil CO2 efflux, except at a~hydric shrubland where drought tended to increase soil respiration. When comparing the fractional importance of each greenhouse gas to the total numerical global warming response, the change in CO2 efflux dominated the response in all treatments (ranging 71–96%), except for NO3− addition where 89% was due to change in CH4 emissions. Thus, in European peatlands and shrublands the feedback to global warming induced by the investigated anthropogenic disturbances will be dominated by variations in soil CO2 fluxes.

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