This study investigates the decades-long evolution of groundwater dynamics and thermal field in the North German Basin beneath Brandenburg (NE Germany) by coupling a distributed hydrologic model with a 3D groundwater model. We found that hydraulic gradients. acting as the main driver of the groundwater flow in the studied basin. are not exclusively influenced by present-day topographi... https://www.theirrationaleconomist.com/product-category/quickstrikes/