Ocean Circulation and Climate: Observing and Modelling the Global Ocean
Feb 18, 2010
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A physicist and physical oceanographer discusses the challenges of predicting ocean circulation dynamics, exploring the impact of eddies on glacial cycles and the Gulfstream shutdown. The podcast delves into ocean system complexity, advancements in observation methods, and experimental models unraveling ocean dynamics. The discussion also touches on ocean overturning circulation, climate implications, and the difficulties in predicting abrupt changes in ocean and atmospheric temperatures.
The complexity of ocean circulation systems poses challenges for predicting their evolution due to vast scales and limited sampling.
Improvements in ocean observation technologies like satellite altimeters and argo floats enhance understanding of oceanic processes.
Predicting future changes in ocean circulation is hindered by uncertainties in attributing variations to forcing mechanisms and the system's sensitivity.
Deep dives
Overview of Complex Ocean Circulation Systems
The podcast delves into the intricate dynamics of ocean circulation systems, highlighting the vast complexity and scale of these systems. It discusses the interplay between various factors like surface circulation, gyres, and overturning circulation, emphasizing the importance of ocean eddies and their impact on global motion. The speaker presents a thorough analysis of how ocean circulation influences climate observing and modeling at a global level.
Challenges in Observing and Modeling the Global Ocean
The podcast explores the challenges associated with observing and modeling the global ocean due to its sheer size, remoteness, and opaqueness to electromagnetic radiation. It discusses historical methods of hydrographic monitoring and highlights improvements in ocean observation technologies, such as satellite altimeters and argo floats. The speaker emphasizes the importance of time series data and process experiments to enhance understanding of oceanic processes.
Implications of Ocean Circulation Changes
The podcast provides insights into the potential implications of changes in ocean circulation, focusing on scenarios like the weakening of the Atlantic overturning circulation. It discusses the relationship between surface air temperatures, sea surface temperatures, and the Atlantic multi-decadal oscillation, highlighting the uncertainties and complexities involved in attributing changes in circulation to varying forcing mechanisms.
Predictability and Predictive Models
The podcast touches on the concept of predictability in oceanic systems, exploring the potential for model predictions based on historical and current data. It examines the sensitivity of the overturning circulation to thermal and atmospheric forcing patterns, showcasing the challenges in predicting future changes in the circulation system. The speaker highlights ongoing research efforts to enhance predictive capabilities and understand the variability of ocean circulation.
Key Takeaways and Recommendations
In conclusion, the podcast underscores the importance of combining observational data, simple models, and numerical simulations to gain a comprehensive understanding of ocean circulation systems. It emphasizes the need for caution in sensationalizing scientific findings, particularly regarding tipping points and potential abrupt changes in circulation. The speaker advocates for a balanced and transparent approach to communicating scientific complexities to the public and policymakers for informed decision-making.
The oceans are a critical component of the climate system, storing roughly 1000 times as much heat, and 50 times as much carbon, as the atmosphere. In this talk, Professor David Marshall (21st Century Ocean Institute, University of Oxford) will discuss the challenges of predicting the evolution of a complex system that is grossly under-sampled and spans a bewildering range of scales in both space and time. These challenges will be illustrated through the important but over-sensationalised problem of how the Gulf Stream may change over the next century and impacts on European climate.
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