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Conversely, according to other studies (Wang et al. 2001; Yuan et al. 2004), the δ18O of stalagmites from Chinese caves was isotopically light during the late deglaciation, indicating that precipitation increased because of the increased strength of the East Asian summer monsoon at that time.
The report describes the very high probability by the late 21st century of increased temperatures and more heat waves over most land areas; increased frequency, intensity, and/or amount of heavy precipitation; increased intensity and duration of drought; increased intense tropical cyclone activity; and increased extreme high sea level.
A noteworthy departure from existing norms occurred from the 16th to the 18th century, the period of the so-called Little Ice Age in Europe: precipitation increased significantly along the tropical margin of the Sahara, in the desert itself, and perhaps along the northern margin as well.
The phosphate content decreased as the pH of precipitation increased.
The Ni3P precipitation increased wear loss and the friction coefficient.
Precipitation increased significantly from Africa to Americas and Australasia and then to Asia.
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The magnitude of precipitation trend and the numbers of GCM with a precipitation increasing increase gradually with time.
Precipitation increases the critical nucleation diameter and the resulting grain size.
Summer precipitation will change steadily due to global warming with the annual average precipitation increasing 19% by the last 30 years of the 21st century.
And similar to rainy days, monthly maximum precipitation and monthly precipitation, increasing trend in the first half of a year is stronger than that of the second half of a year.
That could become a serious problem when precipitation increases due to climate change and spikes the probability of air and water socializing with long-frozen tailings.
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CEO of Professional Science Editing for Scientists @ prosciediting.com