IWRM

Integrated Environmental Management Course (SE Solutions)

University of the Free State (Venue: Equitas Building), Bloemfontein
  • IWRM
  • Environmental management

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Integrated Environmental Management Course (SE Solutions)

University of the Free State (Venue: Equitas Building), Bloemfontein

Climate Services Policy Dialogue: Towards Implementation of the National Framework for Climate Services in South Africa

  • Climate
  • IWRM
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Climate Services Policy Dialogue: Towards Implementation of the National Framework for Climate Services in South Africa

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Using Hydrogeologic Conceptual Model To Implement A Successful Iwrm Approach In Limphasa River Catchment, Malawi

This study examined the effective use of the hydrogeologic conceptual model (HCM) to implement the integrated water resource management (IWRM) approach. While research focuses on using hydrogeologic models  in  groundwater  for  planning,  few  studies  show  how  to  use  HCM  for  a successful IWRM approach, especially in  resource  poor  catchments.  This  is  largely  due  to  t he lack of adequate data to showcase such models.

A framework for conjunctive use at local government level

Conjunctive use of surface water and groundwater resources offers huge advantages to municipalities. It can significantly increase the resilience of the municipal water supply to drought situations. Optimal use and integration of different sources would result in a yield of the total system that is higher than the combined yield of each source separately. However, integrated water resource management (IWRM) in general and planned conjunctive use of both groundwater and surface water resources in particular have not been successfully implemented yet in South Africa.

Quantifying Groundwater Resources In Alluvial Aquifers Of The Omaruru River; Simplifying Decision Making For Aquifer Management

The Omaruru River Basin encompasses an area of approximately 19 625 km2 in central west Namibia. The headwaters extend to the area north of the Etjo Mountains, ephemeral surface runoff and groundwater flow is generally directed south-westward until they reach the Atlantic Ocean. Annual rainfall decreases steadily from 380 mm at the headwaters to <50 mm at the river mouth implying that majority of runoff is generated in the upper headwaters.