
NSF Org: |
RISE Integrative and Collaborative Education and Research (ICER) |
Recipient: |
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Initial Amendment Date: | August 29, 2018 |
Latest Amendment Date: | August 20, 2020 |
Award Number: | 1824770 |
Award Instrument: | Standard Grant |
Program Manager: |
Richard Yuretich
RISE Integrative and Collaborative Education and Research (ICER) GEO Directorate for Geosciences |
Start Date: | August 15, 2018 |
End Date: | September 30, 2024 (Estimated) |
Total Intended Award Amount: | $1,301,722.00 |
Total Awarded Amount to Date: | $1,301,722.00 |
Funds Obligated to Date: |
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History of Investigator: |
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Recipient Sponsored Research Office: |
150 MUNSON ST NEW HAVEN CT US 06511-3572 (203)785-4689 |
Sponsor Congressional District: |
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Primary Place of Performance: |
170 Whitney Ave New Haven CT US 06520-8118 |
Primary Place of
Performance Congressional District: |
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Unique Entity Identifier (UEI): |
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Parent UEI: |
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NSF Program(s): |
ECOSYSTEM STUDIES, DYN COUPLED NATURAL-HUMAN |
Primary Program Source: |
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Program Reference Code(s): |
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Program Element Code(s): |
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Award Agency Code: | 4900 |
Fund Agency Code: | 4900 |
Assistance Listing Number(s): | 47.050 |
ABSTRACT
This project examines the link between explosive volcanic eruptions and the annual Nile river summer flooding in antiquity. Large volcanic eruptions can reduce average global temperatures and suppress average global precipitation. This is known to have had dramatic effects on annual rainfall on the Nile watershed in historic times. The human response to this annual flooding, and to its variability over the years, was the major driver of Egyptian history up to the completion of the high dam at Aswan in 1970. This project, a collaboration among historians, scientists, hydrologists, and statisticians, seeks to understand the coupling between the hydrological cycle and human society in Egypt during the Hellenistic era (305 BCE - 30 BCE), a well-documented period of economic, technological and social change with often violent rivalries between major regional powers. The results will also inform our understanding of best-practice responses to the changing climate in the modern world. The project will inform the broad public about human and natural systems and the complex interactions between them at diverse scales, through a traveling exhibition program developed at the Yale Peabody Museum of Natural History.
This project will capitalize upon a rare confluence of natural and human archives for Ancient Egypt and the Near East. By comparing rich historical records (papyrus documents and inscriptions) with environmental data and regional climate and hydrologic simulations for repeated abrupt climate events, the research will determine whether and how social dynamics are climate-driven, and whether and how human water management affects regional climate and hydrology. Volcanic eruptions provide tests of human and natural system sensitivity to abrupt shocks because their repeated occurrence allows the identification of systematic relationships in the presence of random variability. The project will make three important contributions: (1) integrate historical data from a wealth of different archives to analyze the connections between climate variability, social unrest, and institutional change during the Hellenistic era; (2) improve knowledge of hydrological responses to volcanic eruptions; (3) document the extent of human impacts on Mediterranean hydrology. Simulations will be used to evaluate the climatic impact of large and sustained volcanism and intensive regional water management. This historical analysis will delineate the mechanisms through which environmental stress influenced state-level behaviors, community responses (such as changes in land and water management), and interstate conflict during the Hellenistic period, and how in return human activities interactively affected soils, land cover, hydrology, and regional climate.
This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.
PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH
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PROJECT OUTCOMES REPORT
Disclaimer
This Project Outcomes Report for the General Public is displayed verbatim as submitted by the Principal Investigator (PI) for this award. Any opinions, findings, and conclusions or recommendations expressed in this Report are those of the PI and do not necessarily reflect the views of the National Science Foundation; NSF has not approved or endorsed its content.
The project’s multidisciplinary team made important contributions in several areas, including: (1) the integration of historical data from a wealth of different archives, to detail and explain the connections between climate variability, social unrest, and institutional change during the Ptolemaic era in Egypt, 305-30 BCE (e.g., McConnell et al., 2020; Ludlow and Manning, 2021; Izdebski et al., 2022) and; (2) improved understanding of global and regional (including Nile Basin) climatic and hydrological responses to volcanic eruptions (e.g., McConnell et al., 2020; Singh et al., 2023).
A graduate student at Yale working on the project, Joe Morgan, led the creation of a database of both Greek and Egyptian language sources that is five times larger and covers nearly every year of the Ptolemaic period. A key feature of this database is the geocoding of most of the sources, allowing their mapping and (for the first time) integration with a hydrological model of the floodplain.
Model simulations show that commonly flooded areas neatly surrounded most recorded locations of interest during the Ptolemaic period, providing some historical validation (Fig. 1). Flood simulations also showed that agriculture in the Thebaid, the upstream portion of the Egyptian Nile, would have been more sensitive to moderate droughts (Figs. 1 and 2). The downstream Nile, while relatively unaffected during moderate droughts, would have experienced catastrophic loss of irrigated land only during the most severe droughts. Climate simulations by the project team show that the four large and closely timed volcanic eruptions occurring between 168 and 158 BCE would have produced several severe drought years,
A hydrologic model ("Nile River basin) was calibrated using a series of recovered hydrologic records. Manuscripts explaining the calibration of the model and the digitization of hydrologic records are currently being developed.
A computationally inexpensive coupling framework has been developed and implemented in the NASA GISS ModelE to account for vegetation–climate feedbacks during the 2.5 ka period (Singh et al., 2024). This work explores the importance of various performance metrics that can influence vegetation–climate feedbacks and evaluates a set of control climate conditions for the 2.5 ka period against multiproxy paleoclimate reconstructions. Additional ongoing efforts focus on examining the sensitivity of regional climate to various land-use and land-cover changes and using a crop model to analyze the impacts of NASA GISS model–simulated climate conditions on crop yield.
Hundreds of school children from New Haven visit the museum and begin their tour right in front of our display (Public Display).
Izdebski, A., Bloomfield, K., Eastwood, W. J., Fernandes, R., Fleitmann, D., Guzowski, P., Haldon, J., Ludlow, F., Luterbacher, J., Manning, J. G., Masi, A., Mordechai, L., Newfield, T. P., Stine, A. R., Senkul, C. and Xoplaki, E. (2022), "The Emergence of Interdisciplinary Environmental History: Bridging the Gap between the Humanistic and Scientific Approaches to the Late Holocene," Annales, 77(1), 11-58. DOI:10.1017/ahss.2022.114
Ludlow, F. and Manning, J. G. (2021) “Volcanic Eruptions, Veiled Suns, and Nile Failure in Egyptian History: Integrating Hydroclimate into Understandings of Historical Change”, In: Erdkamp, P., Manning, J. G. and Verboven K. (eds.), Climate Change and Ancient Societies in Europe and the Near East: Diversity in Collapse and Resilience. London: Palgrave Macmillan, 301-320. DOI: 10.1007/978-3-030-81103-7_10
Manning, J. G., Ludlow, F., Stine, A. R. Boos, W., Sigl, M. and Marlon, J. (2017) “Volcanic Suppression of Nile Summer Flooding Triggers Revolt and Constrains Interstate Conflict in Ancient Egypt”, Nature Communications, 8, Article 900. doi: 10.1038/s41467-017-00957-y
McConnell, J. R., et al. (2020) “Extreme Climate after Massive Eruption of Alaska’s Okmok Volcano in 43 BCE and Effects on the late Roman Republic and Ptolemaic Kingdom”, Proceedings of the National Academy of Sciences, 117 (27), 15443-15449. DOI:10.1073/pnas.2002722117
Sigl, M., Winstrup, M., McConnell, J.R., Welten, K.C., Plunkett, G., Ludlow, F., Büntgen, U., Caffee, M., Chellman, N., Dahl-Jensen, D., Fischer, H., Kipfstuhl, S., Kostick, C., Maselli, O.J., Mekhaldi, F., Mulvaney, R., Muscheler, R., Pasteri, D.R., Pilcher, J.R., Salzer, M., Schüpbach, S., Steffensen, J.P., Vinther, B., Woodruff, T.E. (2015) "Timing and Climate Forcing of Volcanic Eruptions during the Past 2,500 years", Nature, 523, 543-549, doi:10.1038/nature14565.
Singh, R., Kostas, T., LeGrande, A. N., Ludlow, F. and Manning, J. G. (2023) “Investigating Hydroclimatic Impacts of the 168–158 BCE Volcanic Quartet and their Relevance to the Nile River Basin and Egyptian History”, Climate of the Past, 19 (1), 249-275. DOI:10.5194/cp-19-249-2023.
Singh, R., Koch, A., LeGrande, A. N., Tsigaridis, K., Ramos, R. D., Ludlow, F., Aleinov, I., Ruedy, R., and Kaplan, J. O. (2024): Modelling framework for asynchronous land-atmosphere coupling using NASA GISS ModelE and LPJ-LMfire: Design, Application and Evaluation for the 2.5ka period. Geosci. Model Dev. Discuss. [preprint], https://doi.org/10.5194/gmd-2024-219, in review, 2024.
Last Modified: 02/17/2025
Modified by: Joseph G Manning
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