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UrduThis work, which was supported by the National Science Foundation, was published today in the journal Science Advances.
WHOI Assoc. Scientist Caroline Ummenhofer and MIT-WHOI Joint Program student Theo Carr co-authored the study, along with lead author Rhawn Denniston, professor of Geology at Cornell College and WHOI adjunct scientist, and colleagues from Iowa State University and the University of New Mexico.
The team reconstructed changes in monsoon rainfall over the last 1,500 years using the chemistry of stalagmites from a cave in the Australian tropics. The stalagmites were dated using the small amounts of radioactive isotopes they contain, and variations in monsoon rainfall were determined from changes in the stalagmites’ isotopes of oxygen.
The resulting record turned out to be strikingly similar to a previously published record of tropical cyclone activity from much further south in the Australian subtropics: when the tropics got more rainfall from the monsoon, the subtropics got more rainfall from tropical cyclones.
“That didn’t make any sense to me at first because what happens in the tropics with the monsoon should be distinct from what happens with cyclone activity in the subtropics,” Denniston said. “The only thing I could think of that would connect the two is the ITCZ.”
The ITCZ, or Intertropical Convergence Zone, is a belt of rising air that forms the center of monsoon rainfall in tropical regions around the world. The ITCZ roughly parallels the equator and migrates back and forth between the northern and southern hemispheres, tracking summer heating of the Earth’s surface.
“We compared the tropical cyclone tracks during years that had the ITCZ in a more southerly position with those years when it was located further north,” Ummenhofer added. “We were struck by how different both surface ocean temperatures and actual hurricane tracks over the Indian Ocean were during these two sets of years. A more southerly ITCZ position meant warmer ocean temperatures and more cyclones near the cave site in northwestern Australia–and hence making landfall further south in Western Australia.”
“There’s a lot of atmospheric disturbance in the ITCZ, and as a result, a lot of tropical cyclones form there,” Denniston continued. “The connection we made was that while the ITCZ moves into the southern hemispheres at the start of the austral summer each December, it doesn’t always park itself in the exact same place. When you look at it over hundreds and thousands of years, like we did using our stalagmite records, larger scale patterns are evident; some years the ITCZ stays closer to the equator and when it does, the Australian tropics receive less monsoon rainfall. Other times the ITCZ migrates much further south, increasing monsoon rainfall across tropical regions. We wondered if in those years when the ITCZ was further south if cyclones were forming further south as well, causing more of them to pass over the subtropics, delivering more rain there.”
To test this hypothesis, the team partnered with experts in the study of the ITCZ–Dr. Francesco Pausata and his graduate student, Roberto Ingrosso, of the University of Quebec. They examined climate data based both on observations and a climate model simulation of the last millennium to identify years when the southern hemisphere ITCZ was positioned either particularly far north or south. Next, Dr. Caroline Ummenhofer of the Woods Hole Oceanographic Institution compared tropical cyclone tracks over Australia during recent years.
And finally, MIT Professor Kerry Emanuel applied a cutting-edge simulation of hurricanes to the observational and climate model data to test how changes in the location of the ITCZ impacted tropical cyclone rainfall over the Australian subtropics.
“The stalagmites, modern cyclone tracks, and climate model simulations agreed beautifully,” Denniston said. “When the ITCZ was further south, the tropics got more rainfall from the monsoon and the subtropics got more rainfall from tropical cyclones.”
How is your research different?
“Our study is unique in its ability to demonstrate how closely tied monsoons and tropical cyclones are to the ITCZ over long periods of time. The whole system is so noisy that we can’t make a lot of sense of it over the short record (about 40 years) of direct observations and measurements,” Denniston said. “However, by combining stalagmite records and climate model simulations, we can see how things operate over much longer time periods. What is revealed is that cyclones and monsoons varied in tandem at a really fine scale.”
What does this mean for climate change?
“A really important question in climate science involves the so-called ‘widening of the tropics,’ in which dry air is expanding toward higher latitudes across the subtropics. The southern portions of Australia, where most Australians live and where most of their farmland is located, appear to be particularly at risk of suffering increased droughts due to this phenomenon,” Denniston said. “One possible conclusion of our work is that the same shifts in climate that are causing central and southern Australia to become drier may also lead to more frequent rainfall events from cyclones. Australia is a drought-sensitive country and has suffered massive and extended droughts numerous times over the last 120 years. As this region’s climate is already teetering on the edge, continued drying could spell major problems for agriculture, society, and the environment. However, more regular big rainfall events from tropical cyclones could potentially help offset some of the long-term drying.”
What does this mean for the future?
“This work is an illustration of how the climate system is composed of lots of interlocking pieces. Changes in the ocean and atmospheric temperatures can influence the location of the ITCZ, which in turn influences the monsoon rains in the Australian tropics and the rains derived from tropical cyclones in the much drier regions further south,” Denniston said. “Our study also shows the power of combining geologic records of past climate with climate model simulations. We really need to understand all the pieces of the puzzle to prepare for the climate changes that are coming, and this approach is a great way to do it.”
In addition to the National Science Foundation, funding for this study was provided by the WHOI Independent Research & Development Program and the James E. and Barbara V. Moltz Fellowship.
About Woods Hole Oceanographic Institution
The Woods Hole Oceanographic Institution (WHOI) is a private, non-profit organization on Cape Cod, Massachusetts, dedicated to marine research, engineering, and higher education. Established in 1930, its primary mission is to understand the ocean and its interaction with the Earth as a whole, and to communicate an understanding of the ocean’s role in the changing global environment. WHOI’s pioneering discoveries stem from an ideal combination of science and engineering—one that has made it one of the most trusted and technically advanced leaders in basic and applied ocean research and exploration anywhere. WHOI is known for its multidisciplinary approach, superior ship operations, and unparalleled deep-sea robotics capabilities. We play a leading role in ocean observation and operate the most extensive suite of data-gathering platforms in the world. Top scientists, engineers, and students collaborate on more than 800 concurrent projects worldwide—both above and below the waves—pushing the boundaries of knowledge and possibility. For more information, please visit www.whoi.edu
