Historically, the Regge was a free-flowing shallow lowland river which meandered through a landscape containing marshes, wet meadows and sandy levees. To facilitate shipping, from 1848 onwards the river was straightened by cutting off meanders, and the river channel was deepened and widened. Dams were built to better regulate the river flow, and the floodplain was embanked to protect the adjacent land from flooding. In 1935, the river was almost completely canalised, reducing its length from roughly 70 km to 50 km.
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Las Tablas de Daimiel National Park is a protected natural space, a unique Mediterranean wetland of great natural and cultural value due to the hydrographic basin and geology on which it sits. The confluence of two rivers in an area of minimum slope causes their waters to overflow, which together with the underground contribution of a large aquifer leads to the formation of a puddled river zone: the fluvial flats.
Author of the picture: Guillermo Cobos Campos/Fototeca CENEAM
Until the 70s, the lower course of the Arga River near the confluence with the Aragon River flowed with a meandering channel, occupying a wide flood plain characterized by intense fluvial dynamics. In this situation, it was considered necessary to carry out works to contain river floods, by rectifying and channel the section stretching from the town of Falces to the mouth of the Aragón River.
In the framework of the LIFE AgriAdapt project, more than 120 pilot farms are testing sustainable adaptation measures to enhance the farm resilience to climate change, reduce greenhouse gas emissions and improve the farm competitiveness.
AgriAdapt project, more than 120 pilot farms are testing sustainable adaptation measures to enhance the farm resilience to climate change, reduce GHGs emissions and improve the farm competitiveness.
Herdade do Freixo do Meio is an organic certified farm of 440 hectares located in the Alentejo region in the south of Portugal, a region characterized by the multifunctional agro-silvo-pastoral system of cork and holm oak trees, named montado. This farm employs about 20 people and produces cork, vegetables, fruit, wine and herbs, and holds animals (such as sheep, cows, pig, turkey and chicken) extensively.
The increasing exposure to floods is a consequence of the river regulation and land reclamation works that shaped the landscape in the Tisza River floodplain. During the last 150 years an extensive flood defence and water management infrastructure has been constructed. Climate and land use change in the basin are increasing the frequency and magnitude of floods. The Hungarian Government has been pursuing a new flood defence strategy for the Tisza based on temporary reservoirs where peak flood-water can be released.
The Segura River Basin in the south east of Spain suffers from a structural condition of water scarcity and drought occurrence. For decades, the focus for dealing with this condition has been placed on instrumental objectives such as increasing water transfer facilities (i.e. Tagus Segura Water Transfer, a major diversion project), developing alternative sources (i.e. desalination and reuse) or making use of water in a more technically efficient way (i.e. irrigation modernization).
The Regge River is a typical rain fed river. Starting in the 19th century the first bends were cut and over the years the Regge River was largely turned into a canal. In situations with heavy rainfall, large areas in the valley of the river are flooded. In dry periods, on the contrary, agriculture and the wetlands suffer from the lack of water. Because of climate change, precipitation is projected to become more extreme; showers heavier and dry spells more prolonged. Measures directed at restoring the dynamics of the river must also help to adapt to these projected changes.
Tamera, a farm of 154 ha, is located in the most arid region of Portugal (Alentejo). This area has shown significant trends of increasing erosion and desertification. Only a few decades ago, the Alentejo was a region where the streams flowed with water all year round, even in summer. Today the streams swell only during the rainy season and afterward they become dry again. The system has fallen completely out of balance and climate change is expected to exacerbate the situation.