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Attema, J. J., Loriaux, J. M. & Lenderink, G. Extreme precipitation response to climate perturbations in an atmospheric mesoscale model.
Chung, C. T. Y. & Power, S. B. Precipitation response to La Niña and global warming in the Indo-Pacific.
Chung, C. T. Y., Power, S. B., Arblaster, J. M., Rashid, H. A. & Roff, G. L. Nonlinear precipitation response to El Niño and global warming in the Indo-Pacific.
Although arid conditions associated with such a shift are well documented in southern Asia, as far south as Borneo, debate still exists regarding the precipitation response in southern Indonesia and Australia during HS1.
Although modeled precipitation response remains uncertain, extremes are likely to increase (see " Climate Change Projections").
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Liu, F. et al. Global monsoon precipitation responses to large volcanic eruptions.
Liu, C. & Allan, R. P. Observed and simulated precipitation responses in wet and dry regions 1850-2100.
Barnes, E. A., Solomon, S. & Polvani, L. M. Robust wind and precipitation responses to the Mount Pinatubo eruption, as simulated in the CMIP5 models.
During strong, positive (i.e. El Niño) ENSO phases, the global land area as a whole receives less-than-normal P as shown in Fig. 4, despite that precipitation responses to El Niño events may differ in different regions.
Evidence of middle Holocene aridity in eastern Tennessee and western North Carolina contrasts with evidence of mesic conditions on the ACP, a geographic pattern similar to modern teleconnected precipitation responses to the Pacific Decadal Oscillation.
Berg, P., Moseley, C. & Haerter, J. O. Strong increase in convective precipitation in response to higher temperatures.
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