The contribution of Space Technologies to Arctic Policy Priorities
This report compares the needs of Arctic stakeholders (as articulated in policies and strategies) with the contribution different types of satellite technologies (communications, weather, navigation, earth observation, surveillance, and science) can make to meet current and future requirements. It will help the European Space Agency (ESA) understand Arctic issues, increase the synergy betwee ...
Protecting Arctic Biodiversity: Limitations and strengths of environmental agreements
The Arctic region is characterized by some of the largest continuous intact ecosystems on the planet, but is facing increasingly larger threats. These threats include the full range of stressors known from other parts of the world, namely habitat loss and fragmentation from infrastructure and industrial development, chemical pollution, overharvesting, climate change and invasive species infe ...
Arctic Biodiversity Trends 2010: Selected indicators of change report
Unique Arctic habitats for flora and fauna, including sea ice, tundra, lakes, and peatlands have been disappearing over recent decades, and some characteristic Arctic species have shown a decline. The changes in Arctic Biodiversity have global repercussions and are further creating challenges for people living in the Arctic.
Many Strong Voices - Turning Vulnerability into Strength
Climate change presents the human race with profound choices that go beyond the current debate over new technologies, economic, and social costs and even concerns over environmental impacts. UN Secretary General Ban Ki-moon has called climate change the “moral imperative and the defning issue of our era.”
Global Outlook for Ice & SnowThe “Global Outlook for Ice & Snow” is a special and unique UNEP report launched to mark World Environment Day on 5 June 2007. Snow and ice, with their large areas but relatively small volumes, are inextricably connected to key interactions and responses in the global ecosystem, including solar reflectivity and ocean circulation.