Large-Scale Assessment of Symbiotic Dinitrogen Fixation by Crops: Soybean and Alfalfa in the Mississippi River Basin

2004 ◽  
Vol 96 (6) ◽  
pp. 1754-1760 ◽  
Author(s):  
Michael P. Russelle ◽  
Adam S. Birr
2021 ◽  
Vol 13 (8) ◽  
pp. 1590
Author(s):  
Cassandra Nickles ◽  
Edward Beighley

The upcoming Surface Water and Ocean Topography (SWOT) mission will measure rivers wider than 50–100 m using a 21-day orbit, providing river reach derived discharges that can inform applications like flood forecasting and large-scale hydrologic modelling. However, these discharges will not be uniform in time or coincident with those of neighboring reaches. It is often assumed discharge upstream and downstream of a river location are highly correlated in natural conditions and can be transferred using a scaling factor like the drainage area ratio between locations. Here, the applicability of the drainage area ratio method to integrate, in space and time, SWOT-derived discharges throughout the observable river network of the Mississippi River basin is assessed. In some cases, area ratios ranging from 0.01 to 100 can be used, but cumulative urban area and/or the number of dams/reservoirs between locations decrease the method’s applicability. Though the mean number of SWOT observations for a given reach increases by 83% and the number of peak events captured increases by 100%, expanded SWOT sampled time series distributions often underperform compared to the original SWOT sampled time series for significance tests and quantile results. Alternate expansion methods may be more viable for future work.


2021 ◽  
pp. 205301962198908
Author(s):  
Derek Hoeferlin

Designers have a three-part responsibility owed to their object of study: to appreciate, to speculate, and to collaborate. This is particularly true for the professional engagement with spaces on the scale of river basins which impact and prioritize certain design decisions on a whole different level. Adequate responses to the ongoing transformations brought forward by large-scale anthropogenic stressors across entire river systems cannot continue to be dominated with hardline and static interventions. Rather, there is a need for alternative outsets, one that begins to design with adaptive and dynamic negotiations. By looking at the example of the Mississippi River Basin, this essay proposes a new integrated water-based design methodology titled “Way Beyond Bigness: The Need for a Watershed Architecture,” an interdisciplinary strategy to rethink the management of river systems for a sustainable future.


2015 ◽  
Vol 16 (2) ◽  
pp. 857-873 ◽  
Author(s):  
Rongqian Yang ◽  
Michael Ek ◽  
Jesse Meng

Abstract Surface water and energy budgets from the National Centers for Environmental Prediction–U.S. Department of Energy (NCEP–DOE) Atmospheric Model Intercomparison Project (AMIP-II) Global Reanalysis 2 (GR2), the North American Regional Reanalysis (NARR), and the NCEP Climate Forecast System Reanalysis (CFSR) are compared here with each other and with available observations over the Mississippi River basin. The comparisons in seasonal cycle, interannual variation, and annual mean over a 31-yr period show that there are a number of noticeable differences and similarities in the large-scale basin averages. Warm season precipitation and runoff in the GR2 are too large compared to the observations, and seasonal surface water variation is small. By contrast, the precipitation in both NARR and CFSR is more reasonable and in better agreement with the observation, although the corresponding seasonal runoff is very small. The main causes of the differences in both surface parameterization and approach used in assimilating the observed precipitation datasets and snow analyses are then discussed. Despite the discrepancies in seasonal water budget components, seasonal energy budget terms in the three reanalyses are close to each other and to available observations. The interannual variations in both water and energy budgets are comparable. This study shows that the CFSR achieves a large improvement over the GR2, indicating that the CFSR dataset can be used in climate variability studies. Nonetheless, improved land surface parameterization schemes and data assimilation techniques are needed to depict the surface water and energy climates better, in particular, the variation in seasonal runoff.


2013 ◽  
Author(s):  
Laura S. Hamilton ◽  
Stephen P. Klein ◽  
William Lorie

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