Evaluating the Effects of Piped Lengths of Buried Channels on Temporal and Small-Scale Spatial Variations of Streams Dissolved Oxygen Dynamics

2020 ◽  
Author(s):  
Mehdi Ketabchy ◽  
Mohammad Nayeb Yazdi ◽  
David Sample ◽  
Durelle Scott
2021 ◽  
Vol 11 (1) ◽  
Author(s):  
Natalie H. N. Low ◽  
Fiorenza Micheli ◽  
Juan Domingo Aguilar ◽  
Daniel Romero Arce ◽  
Charles A. Boch ◽  
...  

AbstractDeclining oxygen is one of the most drastic changes in the ocean, and this trend is expected to worsen under future climate change scenarios. Spatial variability in dissolved oxygen dynamics and hypoxia exposures can drive differences in vulnerabilities of coastal ecosystems and resources, but documentation of variability at regional scales is rare in open-coast systems. Using a regional collaborative network of dissolved oxygen and temperature sensors maintained by scientists and fishing cooperatives from California, USA, and Baja California, Mexico, we characterize spatial and temporal variability in dissolved oxygen and seawater temperature dynamics in kelp forest ecosystems across 13° of latitude in the productive California Current upwelling system. We find distinct latitudinal patterns of hypoxia exposure and evidence for upwelling and respiration as regional drivers of oxygen dynamics, as well as more localized effects. This regional and small-scale spatial variability in dissolved oxygen dynamics supports the use of adaptive management at local scales, and highlights the value of collaborative, large-scale coastal monitoring networks for informing effective adaptation strategies for coastal communities and fisheries in a changing climate.


2000 ◽  
Vol 251-252 ◽  
pp. 497-510 ◽  
Author(s):  
Richard J. Williams ◽  
Craig White ◽  
Martin L. Harrow ◽  
Colin Neal

2008 ◽  
Vol 54 (185) ◽  
pp. 315-323 ◽  
Author(s):  
Helgard Anschütz ◽  
Daniel Steinhage ◽  
Olaf Eisen ◽  
Hans Oerter ◽  
Martin Horwath ◽  
...  

AbstractSpatio-temporal variations of the recently determined accumulation rate are investigated using ground-penetrating radar (GPR) measurements and firn-core studies. The study area is located on Ritscherflya in western Dronning Maud Land, Antarctica, at an elevation range 1400–1560 m. Accumulation rates are derived from internal reflection horizons (IRHs), tracked with GPR, which are connected to a dated firn core. GPR-derived internal layer depths show small relief along a 22 km profile on an ice flowline. Average accumulation rates are about 190 kg m−2 a−1 (1980–2005) with spatial variability (1σ) of 5% along the GPR profile. The interannual variability obtained from four dated firn cores is one order of magnitude higher, showing 1σ standard deviations around 30%. Mean temporal variations of GPRderived accumulation rates are of the same magnitude or even higher than spatial variations. Temporal differences between 1980–90 and 1990–2005, obtained from two dated IRHs along the GPR profile, indicate temporally non-stationary processes, linked to spatial variations. Comparison with similarly obtained accumulation data from another coastal area in central Dronning Maud Land confirms this observation. Our results contribute to understanding spatio-temporal variations of the accumulation processes, necessary for the validation of satellite data (e.g. altimetry studies and gravity missions such as Gravity Recovery and Climate Experiment (GRACE)).


2014 ◽  
Vol 92 ◽  
pp. 566-575 ◽  
Author(s):  
Hong Ling ◽  
Klaus Schäfer ◽  
Jinyuan Xin ◽  
Min Qin ◽  
Peter Suppan ◽  
...  

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