Lecture

Extreme Environments Research: Atmospheric Processes

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Description

This lecture by the instructor focuses on the research conducted at the Extreme Environments Research Laboratory, which specializes in studying regions like the Antarctic, Arctic, Southern Ocean, and the Alps due to their sensitivity to climate change. The lecture delves into the measurement and modeling of atmospheric processes, including chemical composition, microphysics, and cloud processes, emphasizing their impact on Earth's radiative balance and climate change. The instructor explains the complex interactions in polar regions, where feedback loops play a crucial role in understanding how different elements like land, ocean, and cryosphere influence the atmosphere's composition and, consequently, climate. The lecture also covers the methodologies employed, such as conducting measurements in remote areas, utilizing tethered balloon systems for vertical profiling, and analyzing data post-fieldwork to comprehend its implications.

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Related concepts (14)

Climate change

In common usage, climate change describes global warming—the ongoing increase in global average temperature—and its effects on Earth's climate system. Climate change in a broader sense also includes previous long-term changes to Earth's climate. The current rise in global average temperature is more rapid than previous changes, and is primarily caused by humans burning fossil fuels. Fossil fuel use, deforestation, and some agricultural and industrial practices increase greenhouse gases, notably carbon dioxide and methane.

Climate change denial

Climate change denial or global warming denial is dismissal or unwarranted doubt that contradicts the scientific consensus on climate change. Those promoting denial commonly use rhetorical tactics to give the appearance of a scientific controversy where there is none. Climate change denial includes doubts to the extent of how much climate change is caused by humans, its effects on nature and human society, and the potential of adaptation to global warming by human actions.

Politics of climate change

The politics of climate change results from different perspectives on how to respond to climate change. Global warming is driven largely by the emissions of greenhouse gases due to human economic activity, especially the burning of fossil fuels, certain industries like cement and steel production, and land use for agriculture and forestry. Since the Industrial Revolution, fossil fuels have provided the main source of energy for economic and technological development.

Radiative forcing

Radiative forcing (or climate forcing) is the change in energy flux in the atmosphere caused by natural or anthropogenic factors of climate change as measured in watts per meter squared. It is a scientific concept used to quantify and compare the external drivers of change to Earth's energy balance. These external drivers are distinguished from climate feedbacks and internal variability, which also influence the direction and magnitude of imbalance. Positive radiative forcing means Earth receives more incoming energy from sunlight than it radiates to space.

Climate change adaptation

Climate change adaptation is the process of adjusting to the effects of climate change. These can be both current or expected impacts. Adaptation aims to moderate or avoid harm for people. It also aims to exploit opportunities. Humans may also intervene to help adjustment for natural systems. There are many adaptation strategies or options.They can help manage impacts and risks to people and nature. We can classify adaptation actions in four ways. These are infrastructural and technological; institutional; behavioural and cultural; and nature-based options.

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