scholarly journals Evaluation of low-flow metrics as environmental instream flow standards during long-term average and 2016 drought conditions: Tombigbee River Basin, Alabama and Mississippi, USA

Water Policy ◽  
2018 ◽  
Vol 20 (6) ◽  
pp. 1240-1255 ◽  
Author(s):  
Sarah Praskievicz ◽  
Cehong Luo ◽  
Bennett Bearden ◽  
Andrew Ernest

Abstract Environmental instream flows are a common tool for maintaining river flows that are required to sustain both ecosystem and societal needs. Many of the most widely adopted environmental flow standards are based on historical flow, mainly because of the relative simplicity of these methods. Few previous studies, however, have examined the ability of historical flow standards to protect low flows. Here, the low-flow protective ability of five different historical flow methods, using 35 gaging stations in the Tombigbee River Basin of Alabama and Mississippi, was analyzed. The minimum environmental flow thresholds were calculated using the five indices, and the number of times in a recent 32-year period flows fell below each threshold was determined. The Tennant-based threshold was reached most frequently, followed by the modified Tennant. Although other low-flow metrics, such as 7Q10, were triggered infrequently (9% of the time) over the whole period, triggering rates increased to 46% for 7Q10 during the drought of 2016, suggesting that even minimal low-flow standards may provide some benefit during drought. Analyzing historical flow methods to see how often they would result in management actions if implemented is a useful way of developing guidance on the adoption of minimum environmental instream flow standards.

Author(s):  
Jacob Mutua Katuva ◽  
Christian Thine Omuto ◽  
John P. O. Obiero

Lack of water allocation plans in semi-arid river basins increases the risks of hydrological droughts. The Mukurumudzi river basin was experiencing extremely low flows which led to a water allocation assessment to quantify the available resource amidst competing demands from domestic, commercial and environmental needs. An abstraction survey was conducted along the entire length of the river followed by a low flow study and water balance modelling using rainfall-runoff Model. Observed flows at source and mouth were 0.028 m3/sand 0.043 m3/s respectively. Simulated flows estimated an environmental flow (Q95) deficit of0.023 m3/s and 0.010 m3/s in July and August respectively. Normal flow (Q80) of 0.190 m3/s and flood flow (Q50) of 0.520 m3/s were estimated. Compensating the environmental flow deficit in July and August was recommended. A more detailed hydrogeological study should be conducted to elucidate the potential of the groundwater resource in meeting current demands.


2020 ◽  
Vol 117 (21) ◽  
pp. 11328-11336 ◽  
Author(s):  
Justin T. Martin ◽  
Gregory T. Pederson ◽  
Connie A. Woodhouse ◽  
Edward R. Cook ◽  
Gregory J. McCabe ◽  
...  

Across the Upper Missouri River Basin, the recent drought of 2000 to 2010, known as the “turn-of-the-century drought,” was likely more severe than any in the instrumental record including the Dust Bowl drought. However, until now, adequate proxy records needed to better understand this event with regard to long-term variability have been lacking. Here we examine 1,200 y of streamflow from a network of 17 new tree-ring–based reconstructions for gages across the upper Missouri basin and an independent reconstruction of warm-season regional temperature in order to place the recent drought in a long-term climate context. We find that temperature has increasingly influenced the severity of drought events by decreasing runoff efficiency in the basin since the late 20th century (1980s) onward. The occurrence of extreme heat, higher evapotranspiration, and associated low-flow conditions across the basin has increased substantially over the 20th and 21st centuries, and recent warming aligns with increasing drought severities that rival or exceed any estimated over the last 12 centuries. Future warming is anticipated to cause increasingly severe droughts by enhancing water deficits that could prove challenging for water management.


Author(s):  
Jacob Mutua Katuva ◽  
Christian Thine Omuto ◽  
John P. O. Obiero

Lack of water allocation plans in semi-arid river basins increases the risks of hydrological droughts. The Mukurumudzi River Basin was experiencing extremely low flows which led to a water allocation assessment to quantify the available resource amidst competing demands from domestic, commercial, and environmental needs. An abstraction survey was conducted along the entire length of the river followed by a low flow study and water balance modelling using rainfall-runoff model. Observed flows at source and mouth were 0.028 m3/sand 0.043 m3/s, respectively. Simulated flows estimated an environmental flow (Q95) deficit of0.023 m3/s and 0.010 m3/s in July and August, respectively. Normal flow (Q80) of 0.190 m3/s and flood flow (Q50) of 0.520 m3/s were estimated. Compensating the environmental flow deficit in July and August was recommended. A more detailed hydrogeological study should be conducted to elucidate the potential of the groundwater resource in meeting current demands.


2017 ◽  
Vol 8 (1) ◽  
pp. 25-40
Author(s):  
H. H. Heng ◽  
W. F. Pan ◽  
F. L. Siaw ◽  
C. P. Hii

This paper presents an alternative water storage concept at lower sea-river interface vis-à-vis the conventional dam/reservoir storage scheme in the upper headwater region of a river basin. Two (2) estuary or coastal reservoir schemes are proposed to meet the future water demand of Johor Bahru and its vicinity. The low flow yields of a 98% reliability (or design 1:50-year return period) for both river schemes are also presented. A hydrological assessment is carried out to correlate the hydrometric variables, i.e. rainfall and streamflow. A long term 54-year streamflow record is adopted as input to the yield calculation. The reliable yields of 98% reliability criteria are in turn estimated based on a water balance or mass conservation. This new paradigmatic shift of reservoir storage location from headwater region to lower estuary/coastal interface can harness sufficient yield to meet the future demand of Johor Bahru and vicinity.


2007 ◽  
Vol 177 (4S) ◽  
pp. 314-315
Author(s):  
Jose A. Medina Machuca ◽  
Jose A. Medina Coello ◽  
Hugo Manzanilla ◽  
Francisco A. Gutierrez
Keyword(s):  
Low Flow ◽  

Author(s):  
Laima TAPARAUSKIENĖ ◽  
Veronika LUKŠEVIČIŪTĖ

This study provides the analysis of drought conditions of vegetation period in 1982-2014 year in two Lithuanian regions: Kaunas and Telšiai. To identify drought conditions the Standardized Precipitation Index (SPI) was applied. SPI was calculated using the long-term precipitation record of 1982–2014 with in-situ meteorological data. Calculation step of SPI was taken 1 month considering only vegetation period (May, June, July, August, September). The purpose of investigation was to evaluate the humidity/aridity of vegetation period and find out the probability of droughts occurrence under Lithuanian climatic conditions. It was found out that according SPI results droughts occurred in 14.5 % of all months in Kaunas region and in 15.8 % in Telšiai region. Wet periods in Kaunas region occurred in 15.8 %, and in Telšiai region occurrence of wet periods was – 18.8 % from all evaluated months. According SPI evaluation near normal were 69.7 % of total months during period of investigation in Kaunas and respectively – 65.5 % in Telšiai. The probability for extremely dry period under Lithuania climatic conditions are pretty low – 3.0 % in middle Lithuania and 2.4 % in western part of Lithuania.


Think India ◽  
2019 ◽  
Vol 22 (2) ◽  
pp. 296-304
Author(s):  
Biplab Tripathy ◽  
Tanmoy Mondal

India is a subcontinent, there huge no of people lived in river basin area. In India there more or less 80% of people directly or indirectly depend on River. Ganga, Brahamputra in North and North East and Mahanadi, Govabori, Krishna, Kaveri, Narmoda, Tapti, Mahi in South are the major river basin in India. There each year due to flood and high tide lots of people are suffered in river basin region in India. These problems destroy the socio economic peace and hope of the people in river basin. There peoples are continuously suffered by lots of difficulties in sort or in long term basis. Few basin regions are always in high alert at the time of monsoon seasons. Sometime due to over migration from basin area, it becomes empty and creates an ultimate loss of resources in India and causes a dis-balance situation in this area.


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