Award Abstract # 1602629
Collaborative Research: P2C2--Calibrating South East Asian Proxies: Speleothems and Tree-Rings

NSF Org: AGS
Division of Atmospheric and Geospace Sciences
Recipient: THE TRUSTEES OF COLUMBIA UNIVERSITY IN THE CITY OF NEW YORK
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: FY 2017 = $267,428.00
History of Investigator:
  • Brendan Buckley (Principal Investigator)
    bmb@ldeo.columbia.edu
Recipient Sponsored Research Office: Columbia University
615 W 131ST ST
NEW YORK
NY  US  10027-7922
(212)854-6851
Sponsor Congressional District: 13
Primary Place of Performance: Lamont-Doherty Earth Observatory
61 Route 9W
Palisdes
NY  US  10964-1707
Primary Place of Performance
Congressional District:
17
Unique Entity Identifier (UEI): F4N1QNPB95M4
Parent UEI:
NSF Program(s): Paleoclimate
Primary Program Source: 01001718DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 7754, 8070
Program Element Code(s): 153000
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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(Showing: 1 - 10 of 16)
Buckley, B.M., C.C. Ummenhofer, R.D. D?Arrigo, K.G. Hansen, L.H. Truong, C.N. Le and D.K. Stahle "Interdecadal Pacific Oscillation reconstructed from trans-Pacific tree rings: 1350-2004." Climate Dynamics , 2019 https://doi.org/10.1007/s00382-019-04694-4.
Buckley, B.M., C.C. Ummenhofer, R.D. DArrigo, K.G. Hansen, L.H. Truong, C.N. Le and D.K. Stahle "Interdecadal Pacific Oscillation reconstructed from trans-Pacific tree rings: 1350-2004" Climate Dynamics , 2019 https://doi.org/10.1007/s00382-019-04694-4.
Buckley, B.M., K.G. Hansen, K.L. Griffin, S. Schmiege, R. Oelkers, R.D. D'Arrigo, D.K. Stahle, N. Davi, T.Q.T. Nguyen, C.N. Le and R.J.S. Wilson "Blue intensity from a tropical conifer's annual rings for climate reconstruction: An ecological perspective" Dendrochronologia , v.50 , 2018 , p.10 https://doi.org/10.1016/j.dendro.2018.04.003
Buckley, B.M., K. Hansen, K.L. Griffin, S.C. Schmiege, R.C. Oelkers, R.D. DArrigo, D.K. Stahle, N.K. Davi, T.Q.T. Nguyen, C.N. Le and R.J. Wilson "Blue intensity from a tropical conifers annual rings for climate reconstruction: An ecophysiological perspective" Dendrochronologia , v.50 , 2018 , p.10
Li, R., S-Y. Wang, R.R. Gillies, C. Cho, B.M. Buckley and J-H. Yoon "Regional trends in early-monsoon rainfall over Vietnam and CCSM4 attribution" Climate Dynamics , v.26 , 2018
Li, R., S-Y. Wang, R.R. Gillies, C. Cho, B.M. Buckley and J-H. Yoon "Regional trends in early-monsoon rainfall over Vietnam and CCSM4 attribution" Climate Dynamics , v.26 , 2018
Lora R Stevens, Brendan M. Buckley, Sung Kim, Pam Hill, Kelsey Doiron "Increased Effective Moisture in northern Vietnam during the Little Ice Age" Paleo Paleo Paleo , 2018
Lora R. Stevens, Brendan M. Buckley, Sung Kim, Pam Hill, Kelsey Doiron "Increased effective moisture in northern Vietnam during the Little Ice Age" Palaeogeography, Palaeoclimatology, Palaeoecology , 2018 https://doi.org/10.1016/j.palaeo.2018.09.011
Nguyen, H.T.T., S.W.D. Turner, B.M. Buckley and S. Galelli "Coherent streamflow variability in Monsoon Asia over eight centuries - links to oceanic drivers" Water Resources Research , v.56 , 2020 , p.e2020WR02
Rao, M.P., Cook, E.R., Cook, B.I., DArrigo, R., Palmer, J., Lall, U., Woodhouse, C.A., Buckley, B.M., Uriarte, M., Bishop, D.A., Jian, J. and P.J. Webster "Seven centuries of reconstructed Brahmaputra River discharge demonstrate underestimated high discharge and flood hazard frequency" Nature communications , v.11 , 2020 , p.1
Schmiege, S.C., B.M. Buckley, D. Stevenson, C. Truong, N.C. Le and K.G. Griffin "Physiological traits of shade tolerance determine conifer performance in a tropical Vietnamese forest: Lessons from an aberrant flat-leaved pine" Tree Physiology , 2020 10.1093/treephys/tpaa123
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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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