Shallow groundwater–surface water interactions in pond–peatland complexes along a Boreal Plains topographic gradient

Ferone, Jenny-Marie; Devito, K. J.

doi:10.1016/j.jhydrol.2003.12.032

Cited by 180 publications

(228 citation statements)

References 29 publications

Supporting

Mentioning

215

Contrasting

Order By: Relevance

“…To calculate the budget presented above, the tracer ion concentration that is not susceptible to chemical changes and vegetation uptake in lake water should be given to C. Although conservative tracers such as Cland stable isotope have been generally used in many other budget studies (e.g., Drexler et al, 1999;Gurrieri and Furniss, 2004;Hayashi et al, 1998), we adopted Ca 2+ as a tracer ion for comparison of Ca 2+ budgets for two mire pools (Ferone and Devito, 2004). Then, the parameter a for S i in Eq.…”

Section: Chemical Budgetmentioning

confidence: 99%

“…Results show that parameter a tended to decrease in summer and autumn (July-October), apparently reflecting the influence of vegetation growth. Ferone and Devito (2004) estimated the annual budget of Ca 2+ , which was the tracer ion of their hydrological and chemical budgets calculations, for two mire pools in central North America, with errors of 7% and 9% for the observed Ca 2+ storage in lake water. In the present study, Ca 2+ storage was calculated with errors of -19 to 28% for observed values, which were larger than the estimates reported by Ferone and Devito (2004).…”

Section: Evaluation Of Parameter a And Accuracy Of Budget Calculationmentioning

confidence: 99%

“…However, only one study (Ferone and Devito, 2004) has been conducted in North America on hydrological and chemical budgets of mire pools. Furthermore, none has addressed the nutrient budget.…”

Section: Introductionmentioning

confidence: 99%

“…Mire pools developed on kettle-hole peatlands in North America have lower flow rates of water input and output because their hydrological budgets depend on precipitation and evaporation (Ferone and Devito, 2004;Mouser et al, 2005). In contrast, Japanese peatlands have a larger surface water flow rate because of the greater precipitation there than in North America (Nakamura et al, 2002;Yabe and Onimaru, 1997).…”

Section: Introductionmentioning

confidence: 99%

“…Regarding chemical budgets, groundwater flow supplies large shares of chemical constituent inputs (Ferone and Devito, 2004). The chemical constituent flux depends on the groundwater flow rate and the characteristics of soils and rocks under the peat layer, which supplies chemical constituents to the groundwater (Bendell-Young, 2003;Bragazza and Gerdol, 1999;Reeve et al, 1996).…”

Section: Introductionmentioning

confidence: 99%

See 4 more Smart Citations

Hydrological and chemical budgets of a mire pool formed on alluvial lowland of Hokkaido, northern Japan

Kizuka

Yamada

Hirano

2011

Journal of Hydrology

View full text Add to dashboard Cite

Section: Chemical Budgetmentioning

confidence: 99%

Section: Evaluation Of Parameter a And Accuracy Of Budget Calculationmentioning

confidence: 99%

Section: Introductionmentioning

confidence: 99%

Section: Introductionmentioning

confidence: 99%

Section: Introductionmentioning

confidence: 99%

See 3 more Smart Citations

Hydrological and chemical budgets of a mire pool formed on alluvial lowland of Hokkaido, northern Japan

Kizuka

Yamada

Hirano

2011

Journal of Hydrology

View full text Add to dashboard Cite

Arctic terrestrial hydrology: A synthesis of processes, regional effects, and research challenges

et al. 2016

View full text Add to dashboard Cite

Terrestrial hydrology is central to the Arctic system and its freshwater circulation. Water transport and water constituents vary, however, across a very diverse geography. In this paper, which is a component of the Arctic Freshwater Synthesis, we review the central freshwater processes in the terrestrial Arctic drainage and how they function and change across seven hydrophysiographical regions (Arctic tundra, boreal plains, shield, mountains, grasslands, glaciers/ice caps, and wetlands). We also highlight links between terrestrial hydrology and other components of the Arctic freshwater system. In terms of key processes, snow cover extent and duration is generally decreasing on a pan-Arctic scale, but snow depth is likely to increase in the Arctic tundra. Evapotranspiration will likely increase overall, but as it is coupled to shifts in landscape characteristics, regional changes are uncertain and may vary over time. Streamflow will generally increase with increasing precipitation, but high and low flows may decrease in some regions. Continued permafrost thaw will trigger hydrological change in multiple ways, particularly through increasing connectivity between groundwater and surface water and changing water storage in lakes and soils, which will influence exchange of moisture with the atmosphere. Other effects of hydrological change include increased risks to infrastructure and water resource planning, ecosystem shifts, and growing flows of water, nutrients, sediment, and carbon to the ocean. Coordinated efforts in monitoring, modeling, and processing studies at various scales are required to improve the understanding of change, in particular at the interfaces between hydrology, atmosphere, ecology, resources, and oceans.

show abstract

What does it take to flood the Pampas?: Lessons from a decade of strong hydrological fluctuations

Kuppel

Houspanossian

Nosetto

et al. 2015

Water Resources Research

View full text Add to dashboard Cite

While most landscapes respond to extreme rainfalls with increased surface water outflows, very flat and poorly drained ones have little capacity to do this and their most common responses include (i) increased water storage leading to rising water tables and floods, (ii) increased evaporative water losses, and, after reaching high levels of storage, (iii) increased liquid water outflows. The relative importance of these pathways was explored in the extensive plains of the Argentine Pampas, where two significant flood episodes (denoted FE1 and FE2) occurred in 2000-2003 and 2012-2013. In two of the most flood-prone areas (Western and Lower Pampa, 60,000 km 2 each), surface water cover reached 31 and 19% during FE1 in each subregion, while FE2 covered up to 22 and 10%, respectively. From the spatiotemporal heterogeneity of the flood events, we distinguished slow floods lasting several years when the water table is brought to the surface following sustained precipitation excesses in groundwater-connected systems (Western Pampa), and ''fast'' floods triggered by surface water accumulation over the course of weeks to months, typical of poor surface-groundwater connectivity (Lower Pampa) or when exceptionally strong rainfalls overwhelm infiltration capacity. Because of these different hydrological responses, precipitation and evapotranspiration were strongly linked in the Lower Pampa only, while the connection between water fluxes and storage was limited to the Western Pampa. In both regions, evapotranspirative losses were strongly linked to flooded conditions as a regulatory feedback, while liquid water outflows remained negligible.

show abstract

Shallow groundwater–surface water interactions in pond–peatland complexes along a Boreal Plains topographic gradient

Cited by 180 publications

References 29 publications

Hydrological and chemical budgets of a mire pool formed on alluvial lowland of Hokkaido, northern Japan

Hydrological and chemical budgets of a mire pool formed on alluvial lowland of Hokkaido, northern Japan

Arctic terrestrial hydrology: A synthesis of processes, regional effects, and research challenges

What does it take to flood the Pampas?: Lessons from a decade of strong hydrological fluctuations

Contact Info

Product

Resources

About