Effects chain – Example presentation from the ‘soil’ action field

2023 Monitoring Report on the German Strategy for Adaptation to Climate Change

Table of Contents

 

Climate changes relevant to the action field

 

State: Precipitation and drought periods

The picture shows a barren arable field enveloped in warm light emanating from a low sun.
State: Precipitation and drought periods
Source: maxbelchenko / stock.adobe.com

Although the mean precipitation amounts have changed little over recent years, there have been repeated phases regionally of extreme water shortages as well as violent heavy-rain events. Soils can dry out whenever the evaporation in summer increases as a result of high temperatures. Since 2003 there have been particularly frequent incidents of dry phases in summer. As far as heavy-rain events are concerned, high spatial and temporal variability make statistically backed trend statements difficult. However, the general understanding is that heavy rain events have increased as a result of climate change. Especially in warm years, extreme convective precipitation events can occur repeatedly (cf. Changes regarding extremes).

 

Impacts of climate change

 

Impact: BO-I-1 Soil water in agriculturally used soils

The picture shows a sectional view of a maize field with desiccated parts of plants and bare ground. Cracked soil is visible in between the plants.
Impact: BO-I-1 Soil water in agriculturally used soils
Source: Bits and Splits / stock.adobe.com
 

There are critical development phases in the cultivation of agricultural crops which will incur yield losses, if the crops are subject to water shortages during those phases. DWD modelling has demonstrated that the amount of water available to plants during their growth period has diminished in the past 60 years; the trend observed is significant. The decline has been conspicuous above all in the years that have passed since the turn of the millennium.

 

Impact: BO-I-3 Rainfall erosivity

The picture shows raindrops falling on to bare soil. A furrow is visible in the soil.
Impact: BO-I-3 Rainfall erosivity
Source: Inga / stock.adobe.com
 

Given the presumably increasing frequency and intensity of heavy rain events due to climate change, the risk of soil erosion by water is rising. Especially in cases where heavy rain falls on to bare or very dry soils, unable to seep through, this situation can rapidly trigger soil removal processes. In particular, erosion leads to the removal of topsoil, which plays an important role regarding the water retention capacity and the nutrient balance of soils. It takes lengthy and complex processes for this topsoil to be replenished. Erosion weakens the resilience of soils towards climate change while strengthening the associated adverse impacts.

 

Adaptations – activities and results

 

Response: BO-R-2 Permanent grassland terrain

The picture shows grassland with mown grass. The mown grass is lying in rows. In the right-hand margin a tractor can be seen turning hay. In the upper margin you can see a hay bale.
Response: BO-R-2 Permanent grassland terrain
Source: Superingo / stock.adobe.com
 

Under permanent grassland, agriculturally used soils are protected relatively well from adverse impacts of climate change such as erosion or the decomposition of humus. At the same time, moist grassland in particular, helps to stabilise a landscape’s water balance. Since 2013, there has been a precept in force nationwide requiring the conservation of grassland. According to this precept, it is not permitted to plough up grassland unless new grassland is created elsewhere in the territory concerned. Up until 2013 the grassland terrain was diminishing continuously and significantly. After 2013 this trend was reversed. Since then, the grassland terrain and its share of the terrain used for agricultural purposes has been increasing very slowly.

Share:
Article:
Printer-friendly version
Tags:
 2023 Monitoring Report on the DAS