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Published on: June 8, 2015
Westerly jet waviness modulates mid-latitude hydroclimate variability
Liangqing Cheng1, Jingran Zhang2, Yubin Wu3,4
1Key Laboratory of Lake and Watershed Science for Water Security, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing, China.
Mid-latitude hydroclimate variability, driven by westerly jet shifts, increased before 3 million years ago due to Arctic warming. Future global warming may amplify these extremes, threatening vulnerable ecosystems.
Area of Science:
- Paleoclimatology
- Climate Dynamics
- Environmental Science
Background:
- Mid-latitude ecological environments face threats from hydroclimate variability.
- Understanding the drivers of this variability is limited by short observational records and climate model biases.
Purpose of the Study:
- To reconstruct a long-term precipitation record for mid-latitude East Asia.
- To investigate the mechanisms controlling past hydroclimate variability and its future implications.
Main Methods:
- Analysis of a 300.8-meter fluvio-lacustrine sediment core from northern China.
- Development of a sub-millennial resolution precipitation record spanning ~5.7 million years.
- Idealized sensitivity simulations to test hypotheses regarding climate drivers.
Main Results:
- A persistent influence of the westerly jet on mid-latitude precipitation since the Pliocene.
- Reduced mid-latitude precipitation variability after ~3 million years ago, coinciding with amplified low-latitude variability.
- Attribution of pre-3 Ma variability to enhanced westerly jet waviness driven by Arctic warming.
Conclusions:
- Arctic warming historically amplified mid-latitude hydroclimate variability through increased jet waviness.
- Projected future global warming may increase jet waviness, leading to more frequent hydroclimate extremes in mid-latitudes.
- These findings highlight the vulnerability of mid-latitude ecosystems to future climate change.
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