Drought on a global scale

The implications of drought on a global scale are enormous. Not only is the production of food seriously threatened, but other water-related sectors are under pressure as well, such as the supply of drinking water, and cooling for industry and power plants. The environment becomes increasingly threatened, and the risk of forest fires grows. The economic loss caused by drought in the US, for example, is higher than damage caused by other natural disasters such as floods or hurricanes [EPA, 2011]. Industries can be seriously impeded by a lack of cooling water. Hydropower plants are forced to reduce production or even temporarily shut down.

Drought can have various causes. Drought in Southern Europe is mainly caused by a lack of precipitation during winter. Little moisture will be available in the soil and in spring in the first warm period can already lead to drought. This has serious consequences for agriculture and the environment. It must be taken into account that due to climate change, drier winters will occur more often in Southern Europe. [Klein Tank, 2009]

Drought in The Netherlands

Despite heavier rain showers and imminent floods along the rivers, the Netherlands is becoming increasingly drier. In the Netherlands, drought is caused by land reclamation and drainage. Due to the lowering of the water table and drainage or percolation of water, in dry periods there is now a need for water intake. This water is usually of lower quality. Drought in the Netherlands has everything to do with management of the groundwater table.

‘Drought is mainly caused by adaption of the water system to the demand of land use. We discern three categories of causes:

  • drainage and increased expulsion of water for agriculture nationally causes around 60% of drought;
  • ground water extraction for drinking water and industrial use and irrigation cause around 30% of drought; and
  • Other causes, such as an increase in impervious surfaces, forestation (=increase in evaporation) and sand extraction contribute around 10% of the drought causes.’

[Compendium voor de Leefomgeving, 2011]

There is also a difference in distribution; there is a lot of precipitation in winter and little precipitation in summer, which also causes drought (seasonal drought).

The East and South of the Netherlands are irrigated with ground and surface water in times of drought. This water use amounts to some 15% of the total water use in the Netherlands during dry spells.

In the West, only surface water is used for irrigation which is always readily available. Salinisation caused by brackish water seeping in and the intake of foreign salt water is a water quality problem. In dry periods, water is taken in here as well. In the dry spring of 2011, for example, Rijnland let in fresh water from the Stichtse RIjnlanden, though at times of serious drought an irrigation stop is issued.

Drought also brings along with it difficulties for water security. Some 25% of the Dutch flood defence structures consist of peat dikes which contain a lot of water. If this water evaporates, which happens during times of prolonged drought, these dikes can collapse by shifting or sagging. In Wilnis in 2003, a peat dike succumbed and part of the town was flooded. In times of drought these dikes are regularly inspected and in some cases irrigated. In some instances farmers are requested to move their cattle off the dike. [NOS, 2011]


During the drought of 2003, the Dutch Government requested citizens to use drinking water and electricity sparingly. Although provisions were not directly in danger, there was talk of a possible critical situation if the drought were to continue for much longer. A shortage of cooling water could have endangered the electricity production, and the low water level in the rivers eventually would have led to drinking water shortages.

Lower water levels in rivers hinder shipping traffic as waterways become narrower, and as a result of the shallow depth of the rivers only smaller loads can be transported.

In higher parts of the Netherlands such as the sandy soils in the South of the Netherlands, the Veluwe or the Eastern part of the Netherlands, especially in the W+ scenario, groundwater shortages will occur in summertime. For the environment and agriculture this is an imminent problem. It has been calculated that in 2050, with the W+ scenario the South of the Netherlands will have an average shortage of moisture of 400 million m3 in summertime and a lowering of the groundwater table by 10-20 cm. This has major consequences for moisture-loving ecosystems within river catchments and the irrigation for agriculture will increasingly be under pressure. [Rosenboom, 2011]


Due to adjusted water level management and a decrease in drainage and groundwater extraction for drinking water, a part of the drought problems can be remediated. In some bog areas the damage resulting from drainage is irreparable because part of the organic matter has already been oxidized.

An adjustment of the ground water level is not simple, due to the opposite interests of farmers and conservationists. Farmers want the groundwater level to be lowered in spring to prevent the soil from being too damp and soggy so that they can cultivate the land using their farm equipment. Another reason for lowering the water level is that wet soil is colder in spring and crops will grow more slowly.


40% of indigenous plants are threatened by drought. Some fauna such as butterflies and insects are dependent on these plants or a specific humid ecosystem and thus are threatened. The intake of foreign water, usually with a higher fertilizer content, to compensate part of the desiccation causes algal growth, overgrowth of natural areas and dominance of certain species.

In the higher part of the Netherlands it is mainly the decreasing level of seepage of calcium-rich groundwater due to the lowering of the groundwater level because of extraction for drinking water and fast drainage, which is a problem for rare, moisture-loving plant communities and accompanying fauna.

In the lower-lying parts of the Netherlands brackish seepage due to the lowering of the water level and intake of foreign water during dry spells are a threat to flora and fauna, but also to the agricultural sector, which requires fresh water.

In the dunes, groundwater extraction for drinking water is the main cause of desiccation.

Urban drought

With an increase in temperature in cities, evaporation also increases. In the KNMI ’06 scenarios an increase in evaporation of 3 to 15% is indicated for summertime. If this increase in evaporation is not compensated, it will lead to an increase in desiccation. [Klein Tank, 2009]

In urban areas, increasing drought damages vegetation. Most species of grass are not able to stand prolonged periods of drought. Trees and bushes can become seriously or irreparably damaged by prolonged periods of drought. In order to limit these effects on urban green, irrigation is required. This comes at the expense of the already scarce fresh water supply in times of drought.

Prolonged warm and dry periods are often interspersed with heavy rain showers. The dried soil is then not able to absorb much water, which results in overflowing of the sewers after a dry spell with a relatively large effect on the – caused by the drought – vulnerable water system (for example the fish mortality as a result of a lack of oxygen). [Waterschap Hollandse Delta, 2011]

There is a correlation between drought and heat stress, see chapter 5: Heat. In a period of drought the soil and the urban vegetation will no longer emit water vapour (through evaporation). This causes an increase of temperature and problems due to an increase in heat.

With a warming of the climate the need for water sports increases. It will be necessary to ensure the water quality of existing recreational lakes by decreasing the nutrient level in the water. There will also be an increased demand for additional water sports facilities such as water sports objects. With the design and realisation changing circumstances of the urban water system have to be taken into account. If necessary these facilities should be designed with an impermeable bottom to prevent them from falling dry.

A decrease of the groundwater table in cities can lead to damage to building foundations as the top part of  (older) deep foundation piles falls dry (pile rot).

In drier times it is necessary to irrigate many locations in a city to maintain the vegetation.

The interspersed planting of trees in public green areas provides shade for the lower plants preventing excessive evaporation and cooler spots for city dwellers to sit. The trees themselves have deeper roots and are able to provide for their own water supply. Certain tree species are able to stand drought better than others.

In dry periods foreign water is often taken in to prevent damage by drought. The water from outside is often nutrient rich and can also contain salt or pesticides, it can also be turbid and smelly. This can lead to excessive algal growth and a disturbance of water- and plant life.

In the lower-lying parts of the Netherlands salinisation is an extra threat to water quality in the city and consequently also for the flora and fauna. Fresh groundwater will evaporate in longer periods of drought which will not be replenished by rain. This will let seepage flow get stronger or start it up. This process is called internal salinisation; salinisation due to the intake of foreign water is called external salinisation. [Smeets, 2008]