Skip to main content

Science – Society – Technology

Fig. 5 | Geothermal Energy

Fig. 5

From: The interplay of Malm carbonate permeability, gravity-driven groundwater flow, and paleoclimate – implications for the geothermal field and potential in the Molasse Basin (southern Germany), a foreland-basin play

Fig. 5

adapted from the European Project for Ice Coring in Antarctica (EPICA) (Jouzel et al. 2007). Linear scaling for paleo-precipitation forcing is implemented following Seguinot et al. (2018). Red and blue colouring represents mean annual surface temperature above and below zero degrees C, respectively

Paleo-T for a mean annual surface temperature of 9 °C at 300 m altitude

Back to article page