
NSF Org: |
AGS Division of Atmospheric and Geospace Sciences |
Recipient: |
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Initial Amendment Date: | August 23, 2017 |
Latest Amendment Date: | August 23, 2017 |
Award Number: | 1602629 |
Award Instrument: | Standard Grant |
Program Manager: |
David Verardo
AGS Division of Atmospheric and Geospace Sciences GEO Directorate for Geosciences |
Start Date: | September 1, 2017 |
End Date: | August 31, 2020 (Estimated) |
Total Intended Award Amount: | $267,428.00 |
Total Awarded Amount to Date: | $267,428.00 |
Funds Obligated to Date: |
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History of Investigator: |
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Recipient Sponsored Research Office: |
615 W 131ST ST NEW YORK NY US 10027-7922 (212)854-6851 |
Sponsor Congressional District: |
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Primary Place of Performance: |
61 Route 9W Palisdes NY US 10964-1707 |
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): | Paleoclimate |
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 involves a cross-calibration of speleothems and tree rings at two locations in northern and southern Lao PDR at locations uniquely situated to address fundamental questions in tropical paleoclimatology. Such fundamental questions include: What are the relative roles of, and inter-relationships between, the El Nino-Southern Oscillation (ENSO) and the Intertropical Convergence Zone (ITCZ) in influencing Southeast Asian climate variability? Currently, there is no coherent understanding of how the archives from these phenomena reflect climate, specifically how the physical or eco-physiological controls of each influence the stable isotope records extracted from them.
The research team aims to better understand the processes that control the transfer of atmospheric and land surface climate signals to climate proxies by addressing the following questions: 1) How are temperature, precipitation, and stable isotopic variations recorded in the physical, chemical, and biologic signatures of each archive? 2) Are local and regional climate signals synchronous between speleothems and tree rings? and 3) Do the inherent climate signals exhibit inter-proxy variability with seasonal bias or low vs. high frequency variability, and if so, why?
The specific objectives of the research include: i) exploring the dominant controls on and interrelationships between tropical speleothems and tree-rings through a paired cave and tree modern calibration study at two sites in Laos; ii) examining the dominant controls on speleothem and tree-ring stable isotope records for the instrumental period through proxy system modeling and comparison of new and existing records with instrumental climate data and modeled precipitation delta 18 Oxygen; and iii) extending the paleoclimate record back through the last millennium utilizing new and previously collected speleothems and tree cores from North and South Laos.
The potential broader impacts cover three specific areas: research, mentorship, outreach.
On the research side, the project aims to tackle aspects of evolving areas of controversy integrating climate proxies across climate archives and climatic events.
In terms of mentoring, the project supports graduate students during the academic year and undergraduate students in summer research in the Manhattan Center for Science and Mathematics. Students will assist with fieldwork, data processing and analysis, co-authorship of papers, and presentations of results. One of the collaborative institutions, William Patterson University, a Hispanic Serving Institution, is largely a teaching university with a diverse student body that includes many underrepresented minorities that are first generation to college.
Outreach is conducted by all the Collaborators. One of the Principal Investigators is a female Native American scientist and organizes the American Indian Summer Institute in Earth System Science, a two-week residential program for high school students. Another Principal Investigator organizes an annual international Ecological Field School in Vietnam.
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.
Intellectual Merit
We set out to reconstruct past hydroclimatic variability over Mainland Southeast Asia using multiple proxy datasets derived from speleothems and tree-rings, and to compare and calibrate the δ18O records from these two proxy sources. This approach enhanced our ability to investigate the dynamics of Asian monsoon precipitation variability in response to external forcing (e.g., solar), and to natural internal variability governed by coupled ocean-atmosphere processes, such as ENSO. In addition, we sought to investigate how temperature, precipitation, and precipitation isotopic signals are incorporated in each of our respective archives, so that we might better determine whether local and regional climate signals are synchronous or reflective of systematic differences linked to each proxy. We also compared our tree-ring derived hydroclimate indices from Vietnam cypress with a lake sediment δ18O record from northern Vietnam, and demonstrated a coherence in decadal variability for all of the major droughts and pluvials identified in our prior work. The lake sediments, however, allowed for retention of centennial trends in hydroclimate variability that was not possible from tree rings alone, demonstrating the importance of multiple proxy sources. For this project we developed several new δ18O records from existing tree-ring site collections, and used these data for a vastly improved reconstruction of streamflow from the Chao Phraya River, owing to the ability of the stable isotope records to record peak flow. We have expanded this research to a novel way of reconstructing seasonally-discrete streamflow using an improved version of the Monsoon Asia Drought Atlas, and this research continues beyond the current project. We are also continuing with monitoring and analyses of the isotopic variations in rainfall, soil water, cave drip water and for speleothems and tree rings. The research conducted for this project has led to several exciting new avenues for future endeavors.
Broader Impacts
Project PIs traveled to Laos and Vietnam for collection of speleothem and tree ring samples, and during these visits we held two well attended, international workshops at Bidoup Nui Ba National Park in Vietnam. In January 2019 we held Stable Isotopes in the Environment, which was attended by PIs Johnson, Griffith and Buckley, and participants from several countries including the U.K., Australia, Singapore and the USA. In January 2020 we held the first official meeting of the Southeast Asian Paleo Environments Consortium (SAPEC-2020), which was organized by PI Buckley and very well attended by professors and students from multiple countries, with several hands-on instructional sessions. In 2018 we held similar sessions in Laos for the tree ring work in the Nakai Nam Theun region for the work on the rare water pines. From a data standpoint, we have produced a series of robust streamflow reconstructions that include peak season and base flow seasons, and these data will be very useful for regional hydro planning and a variety of other applications. Several graduate student projects were developed during these workshops, especially for Vietnamese students working with project PI Buckley on dendroclimatology and tree ecophysiology within the Annamite Range. This research will form the basis of a course taught by Buckley at Dalat University as part of a Fulbright Award for spring semester 2022 - Predicting the effects of Climate Change on Vietnam's Forests.
Last Modified: 05/07/2021
Modified by: Brendan M Buckley
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