![]() An integration of surface water and groundwater management responses will bring the water table nearer to the surface this could mitigate water storage in the fertile and productive grabens. Striking water level variations in the grabens were linked to rainfall deficit and management scarcity. Importantly, water level fluctuation was faster in streams, springs and hand-dug wells than in boreholes. A water level depletion of up to 2.23 m/year occurred in response to withdrawals in the irrigated plains. The water level of wells varied between horsts and escarpments in the grabens (p <. Spring discharge and streamflow were larger at the foot of the escarpment than at the horst (p <. Spring discharge fluctuates between wet (2.75 ± 1.5 L/s) and dry seasons (0.87 ± 0.21 L/s) (n = 68, p <. Springs (n = 79), stream-flows (n = 48), wetlands (n = 3), endorheic lakes (n = 3), hand-dug wells (n = 48) and boreholes in unconfined aquifers (n = 25) were monitored (2015–2017). We investigated water levels in semi-closed grabens of northern Ethiopia. The findings of the study suggested that both surface water harvesting and groundwater exploitation can be sought in floodplain areas while conserving the uplands. The maximum monthly recharge occurs in September with a recharge value of 78.2 mm. The spatial distribution of simulated runoff was depicted as being higher in the floodplains and along the riparian/drainage lines, whereas upland areas showed lower runoff. Located in the Semien Wollo Zone of the Amhara Region, this town has a longitude and latitude of 1209N 3938E / 12.150N 39.633E / 12.150 39. High flows occur in August, with a median flow of 16.55 m 3 /s and a coefficient of dispersion of 1.55. Kobo (Amharic ) is a town in northern Ethiopia. The monthly low flow occurs in June with a median flow of 1.43 m 3 /s and a coefficient of dispersion of 0.67. The simulated mean annual streamflow at the Basin outlet is 10.6 m 3 /s. The model simulation showed that evapotranspiration accounts for 47% of the input water while surface runoff, lateral flow, and groundwater recharge account for 30%, 1.53%, and 21.4%, respectively. It is found that the multi-variable calibration scenario reasonably attained the minimum satisfactory performance limit for both variables (NSE = 0.67, R 2 = 0.68, PBias = −9.68%, and RSR = 0.57 for calibration of GloFAS flow and NSE = 0.56, R 2 = 0.63, RSR = 0.66, PBias = 3.86 for calibration of MODIS AET). Validated reanalysis river flow from the Global Flood Awareness System (GloFAS) and actual evapotranspiration (AET) from Moderate Resolution Imaging Spectroradiometer (MODIS) were used for single and multi-variable calibration. The main objective of this research is to model the hydrology of the Kobo-Golina catchment using the completely restructured SWAT (SWAT+) model. The role of hydrological models is critically important in rarely studied ungauged catchments including of Kobo-Golina, in the Danakil basin of Ethiopia. Uses the closest city, rather than the more common Eastern,Ĭentral, Mountain or Pacific time zones in the United States.A proper understanding of hydrological processes is vital for water resource assessment, management, and conservation at a local, national, and global scale. Seconds announced at irregular intervals to compensate for theĮarth's slowing rotation. ![]() Seconds defined by International Atomic Time (TAI), with leap ![]() Time (UTC), or Greenwich Mean Time (GMT). Positive or negative offset computed from Coordinated Universal Use it as a meeting planner or a scheduler to find the best time The calculator will automaticallyĪdjust for daylight saving time (DST) in the summer. You can enter airports,Ĭities, states, countries, or zip codes to find the time differenceīetween any two locations. ![]() This is the best time to reach them fromĬonverter for places all over the world. Available Information : Geographical coordinates, Population and Altitude. This will be between 7AM - 11PM their time, since Kobo, Ethiopia is 7 hours ahead of Jackson, Michigan.īut you want to reach someone in Kobo, Ethiopia at work, you may want to try between 2:00 AM and 10:00 AM your time. Kobo : Kobo Localisation : Country Ethiopia, Region Amhara, North Wollo Zone. If you live in Jackson, MI and you want to call a friend in Kobo, Ethiopia, you can try calling them between 12:00 AM and 4:00 PM your time. Schedule a phone call from Jackson, MI to Kobo, Ethiopia ![]() That will end up being between 4:00 PM and 5:00 PM in Kobo, Ethiopia. Meeting at the best time for both parties, you should try between 9:00 AM and 10:00 AM your time in Jackson, MI. Meeting planner for Jackson, Michigan and Kobo, Ethiopia ![]()
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