global climate and are among the fastest warming regions worldwide. It is unclear to what extent anthropogenic environmental changes will impact the structure and functioning of the polar marine ecosystem
change with anthropogenic warming. The adaptation of organisms to these cycles plays an important role in the functionality of ecosystems. With the warming of the Southern Ocean, due to anthropogenic climate
on and use of habitat / improvement of abundance estimates evaluation of possible impacts of anthropogenic activities habitat_modeling.png (Photo: Alfred-Wegener-Institut)
(ROV) as well as laboratory experiments in aquaria at AWI to address the effects of natural and anthropogenic stressors on CWC distribution, health and resilience. Our research contributes to POF-IV Subtopics
determine long-term concentration trends of greenhouse gases and their isotopic compositions and anthropogenic tracers in the background atmosphere. Discover more Technical aspects Results Aerosol measurements
Approaches Towards population Enhancement Find out more OMAP Project: Oysters and mussels under anthropogenic pressure Find out more AI-REEFSHIELD Al-driven Robotic Ecosystem Exploration Framework for Securing [...] environmental research at the AWI Find out more CREATE Project: Concepts for reducing the impact of anthropogenic pressures Find out more Helgoland Oyster Hatchery Technology transfer: European oyster hatchery
MUSES Multi-Use in European Seas Our oceans are faced with ever growing anthropogenic pressures by expanding human activities in offshore areas. This blue growth of marine industries is raising the demand
biomarker-based reconstruction of sea ice, which provides important information on: natural (non-anthropogenically induced) sea ice variability and associated climate variability; Changes in marine primary
Fjords and West Antarctic Peninsula). Glacier melt and retreat are a significant influence of anthropogenic Climate Change on antarctic and subantarctic coastal habitats. As a consequence, increasing amounts
and thus miss a long-term perspective that is, however, crucial for distinguishing natural and anthropogenic triggers for climate change. The present interglacial period, the Holocene and the preceding