Natalie Marie Mahowald | |
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Born | 1963 (age 60–61) |
Alma mater | Massachusetts Institute of Technology University of Michigan Washington University in St. Louis |
Scientific career | |
Institutions | University of California, Santa Barbara Stockholm University Cornell University |
Thesis | Development of a 3-dimensional chemical transport model based on observed winds and use in inverse modeling of the sources of CCl₃F (1996) |
Website | Mahowald Research Group |
Natalie Mahowald (born 1963) is an American Earth scientist who is the Irving Porter Church Professor of Engineering at Cornell University. Her research considers atmospheric transport of biogeochemically-relevant species, and the impact of humans on their environments.
Mahowald studied physics and German at Washington University in St. Louis. She moved to the University of Michigan for her graduate studies, where she earned a master's degree in natural resource policy in 1993. [1] After graduating, Mahowald moved to Germany, where she worked as a consultant on air solution. Mahowald was a doctoral student at Massachusetts Institute of Technology (MIT), where she studied atmospheric sciences. [1] She was a postdoctoral scholar at Stockholm University. [1]
Mahowald was appointed to faculty at the University of California, Santa Barbara. After leaving UCSB, Mahowald joined the National Center for Atmospheric Research (NCAR), where she studied the incorporation of aerosols. [2] She moved to Cornell University in 2007. [3]
Her research considers natural feedbacks in the climate system and how they respond to climate forcings. [1] Amongst these, she has focused on mineral aerosols, fire, the carbon cycle and methane. [1] [4] Aerosols are small particles that cause haze, harm human health and damage air quality. [1] [5] Alongside her work on aerosols, Mahowald has studied soilborne plant pathogens. [6]
In 2017, Mahowald was selected by the United Nations' Intergovernmental Panel on Climate Change (IPCC) to be lead author on the “Special Report on Global Warming of 1.5 degrees Celsius,”. [7] The report evaluated the costs, benefits, tradeoffs and synergies that look to achieve global warming below 1.5 °C. [7] [8] It revealed the finding that a 0.5 °C temperature increase would result in extreme effects on weather events. [9]
Global dimming is a decline in the amount of sunlight reaching the Earth's surface. It is caused by atmospheric particulate matter, predominantly sulfate aerosols, which are components of air pollution. Global dimming was observed soon after the first systematic measurements of solar irradiance began in the 1950s. This weakening of visible sunlight proceeded at the rate of 4–5% per decade until the 1980s. During these years, air pollution increased due to post-war industrialization. Solar activity did not vary more than the usual during this period.
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