[cite=[URL='https://www.bbvaopenmind.com/en/articles/the-impact-of-global-warming-on-the-distribution-of-rainfall-a-historical-perspective/']The Impact of Global Warming on the Distribution of Rainfall: A Historical Perspective | OpenMind[/URL]]
The Impact of Global Warming on the Distribution of Rainfall: A Historical Perspective
Wallace S. Broecker
Columbia University , New York, USA
Model simulations of the response of the Earth to the ongoing global warming predict that the Northern Hemisphere will heat up about twice as fast as the Southern Hemisphere. If so, the thermal equator will undergo a northward shift. By analogy to a shift that occurred about 14.500 years ago, this will strengthen monsoon rains in China, increase the discharge of the Nile, make more arid the dry lands in the 35 to 45º N latitude belt and shift Amazonia to the north. Evidence in support of this prediction comes from the small southwards shift of the thermal equator that accompanied the transition from Medieval Warm to the Little Ice Age.
INTRODUCTION
The changes in rainfall to be generated by the ongoing rise in atmospheric CO2 will likely have the greatest consequences for humans. This will be especially true for the Earth’s dry lands where water is already in short supply. Isaac Held, recipient of the 2012 BBVA climate prize, has predicted based on theory and model simulations that the tropics will get an even larger fraction of global rainfall and that this increase will be at the expense of the adjacent dry lands. Although simulations carried out in linked ocean-atmosphere models confirm Held’s prediction, they disagree widely regarding the details. Because of this, a group that I work with has set out to complement these simulations with evidence gleaned from past climate changes. By past, I mean changes that have occurred during the last 30 thousand years, a time period where radiocarbon dating allows us to correlate events occurring at different places on the planet. As shown in Figure 1, this period includes the Last Glacial Maximum (28 to 18 thousand years ago), the period of deglaciation (18 to 10 thousand years ago) and the Holocene interglaciation (last 10 thousand years). As I will show, two sets of millennium-long punctuations are particularly instructive. One is an oscillation centered at 14.5 thousand years ago (14.5 kyrs) and the other is the Medieval Warm–Little Ice Age oscillation in the latest Holocene.
The article goes into more detail.