The DOI matches its Crossref record; 29 of the 29 references it cites were found in a registry or an index.
Climate Phenomena and their Relevance for Future Regional Climate Change
Abstract
Executive Summary This chapter assesses the scientific literature on projected changes in major climate phenomena and more specifically their relevance for future change in regional climates, contingent on global mean temperatures continue to rise. Regional climates are the complex result of processes that vary strongly with location and so respond differently to changes in global-scale influences. The following large-scale climate phenomena are increasingly well simulated by climate models and so provide a scientific basis for understanding and developing credibility in future regional climate change. A phenomenon is considered relevant to regional climate change if there is confidence that it has influence on the regional climate and there is confidence that the phenomenon will change, particularly under the Representative Concentration Pathway 4.5 (RCP4.5) or higher end scenarios. {Table 14.3} Monsoon Systems There is growing evidence of improved skill of climate models in reproducing climatological features of the global monsoon. Taken together with identified model agreement on future changes, the global monsoon, aggregated over all monsoon systems, is likely to strengthen in the 21st century with increases in its area and intensity, while the monsoon circulation weakens. Monsoon onset dates are likely to become earlier or not to change much and monsoon retreat dates are likely to delay, resulting in lengthening of the monsoon season in many regions .
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Cites
The next generation of scenarios for climate change research and assessment
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A dipole mode in the tropical Indian Ocean
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Increasing drought under global warming in observations and models
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Dai, A. (2011) · WIREs Climate Change · doi:10.1002/wcc.81 · Cited by 3,523 · cited 1×
“Recent downscaling results (Lionello et al., 2008; Evans, 2009; Jin et al., 2010; Dai, 2011) suggest that the eastern Mediterranean will experience a decrease in precipitation during the rainy season due to a northward displacement of the storm tracks (Section 14.”
BackgroundTropical cyclones and climate change
Knutson, T. R., McBride, J. L., Chan, J., Emanuel, K., Holland, G., Landsea, C., Held, I., Kossin, J. P., Srivastava, A. K., & Sugi, M. (2010) · Nature Geoscience · doi:10.1038/ngeo779 · Cited by 3,194
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An overview of the North Atlantic Oscillation
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Cited by
Knutson, T., Camargo, S. J., Chan, J. C. L., Emanuel, K., Ho, C.-H., Kossin, J., Mohapatra, M., Satoh, M., Sugi, M., Walsh, K., et al. (2020) · Bulletin of the American Meteorological Society · doi:10.1175/bams-d-18-0194.1 · Cited by 1,356
Air Quality and Climate Connections
Fiore, A. M., Naik, V., & Leibensperger, E. M. (2015) · Journal of the Air & Waste Management Association · doi:10.1080/10962247.2015.1040526 · Cited by 537
Allen, S. K., Rastner, P., Arora, M., Huggel, C., & Stoffel, M. (2016) · Landslides · doi:10.1007/s10346-015-0584-3 · Cited by 342
Nogueira, M. (2020) · Journal of Hydrology · doi:10.1016/j.jhydrol.2020.124632 · Cited by 279
ENSO Change in Climate Projections: Forced Response or Internal Variability?
Maher, N., Matei, D., Milinski, S., & Marotzke, J. (2018) · Geophysical Research Letters · doi:10.1029/2018gl079764 · Cited by 170
Metadata
- Venue
- Climate Change 2013 – The Physical Science Basis
- Publisher
- Cambridge University Press
- Published
- 2014-03-24
- Pages
- 1217-1308
- OpenAlex
- W1599651335
- Cited by
- 863
- References
- 29
- FWCI
- 141.41
- Type
- book chapter
- Language
- en
- Open access
- closed
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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
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