
NSF Org: |
EAR Division Of Earth Sciences |
Recipient: |
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Initial Amendment Date: | July 2, 2014 |
Latest Amendment Date: | July 24, 2015 |
Award Number: | 1347221 |
Award Instrument: | Continuing Grant |
Program Manager: |
David Lambert
EAR Division Of Earth Sciences GEO Directorate for Geosciences |
Start Date: | July 1, 2014 |
End Date: | June 30, 2018 (Estimated) |
Total Intended Award Amount: | $369,348.00 |
Total Awarded Amount to Date: | $369,348.00 |
Funds Obligated to Date: |
FY 2015 = $254,026.00 |
History of Investigator: |
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Recipient Sponsored Research Office: |
601 S KNOLES DR RM 220 FLAGSTAFF AZ US 86011 (928)523-0886 |
Sponsor Congressional District: |
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Primary Place of Performance: |
Flagstaff Arizona AZ US 86011-0001 |
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): | GEOINFORMATICS |
Primary Program Source: |
01001516DB NSF RESEARCH & RELATED ACTIVIT |
Program Reference Code(s): | |
Program Element Code(s): |
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Award Agency Code: | 4900 |
Fund Agency Code: | 4900 |
Assistance Listing Number(s): | 47.050 |
ABSTRACT
This collaborative grant from the Division of Earth Sciences Geoinformatics program will support the development of software tools which will enable Earth scientists to better quantify and analyze how uncertainties in ages influence records of past climate, ecosystems and landscapes. These tools will allow scientists to better integrate these records, and to integrate larger datasets into predictive models. Thus, the tools will facilitate a more thorough understanding of past climate changes, and more rigorous tests of hypotheses regarding Earth?s history. Two workshops will be held to ensure that the community of scientists who may benefit from these tools are provided with training and opportunities to provide feedback to the software development process.
Specifically, the researchers will develop a package of integrated software tools and make these tools broadly available using the open-source and community supported platform ?R?. The tools will enable paleogeoscientists to use state-of-the-art Bayesian and Monte-Carlo-based approaches to quantifying age uncertainties in paleorecords, and allow more rigorous integration of data sets and models with more thorough accounting for age uncertainties. The tools will allow the broad community of paleogeoscience researchers to visualize and archive their data in intuitive and consistent ways. The researchers will apply the tools to a proof-of-concept data recovery effort aimed at archiving primary geochronological information for marine and terrestrial records of Holocene paleoclimate, thereby providing a synthesis and more permanently archive of results from the NSF Earth System History (ESH) Holocene initiative.
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.
Paleogeoscientists use natural archives to understand how climate, ecosystems, and environments varied prior to human monitoring. Accurately determining the age of samples is critical to this work, allowing scientists to pinpoint phase relationships between Earth systems and their forcings. There is always uncertainty in timing of these records, which can impact the certainty of the results in a number of ways.
The GeoChronR project is all about developing a framework for quantifying and visualizing the impacts of those uncertainties, and creating an easy-to-use set of uncertainty quantification tools for paleogeoscientists.
The single largest barrier to the development of GeoChronR was the lack of an accepted data standard for the paleogeosciences, especially one that could readily include ensembles of geochronologic or paleoenvironmental data. To meet this need, as well as the broader need in the community for a robust and flexible data standard for the paleogeosciences, we developed the Linked PaleoData (LiPD) Framework, a data model and format that is flexible and extensible enough for broad use across the paleogeosciences.
Since we released the LiPD framework in 2016, we have seen broad adoption of the approach and format, having been used in several, large data synthesis efforts in the paleogeosciences, perhaps most notably, in phase 2 of the Past Global Changes temperature of the past 2,000 years project, which assembled nearly 700 records of past temperature change, all in the LiPD format.
The GeoChronR package - a set of software and visualization tools, written in the freely-available and open-source R language, relies on LiPD data for input, output and as a container for age model ensembles. Once the data are loaded in, users can easily create or input age models, perform common analyses, such as correlation, regression, ordination and spectral analysis on the ensembles, and then visualize the output. Examples and tutorials, such as this one for performing ensemble regression (figure 1), http://lipdverse.org/regression.htm, are fundamental documentation for new users seeking to understand the what is possible in GeoChronR. Over the course of the project, we hosted to training workshop for early career researchers at Northern Arizona University. At the workshop, we trained a diverse array of scientists how to use LiPD and GeoChronR. Many of the attendees have made GeoChronR an integral part of their workflow for their scientific projects, and the number of users continues to grow.
GeoChronR, and LiPD, are collaborative projects, that have continued to expand, both in scope and in the number contributors, over the course of the project. We hope that these both continue to expand in the future as we continue to work with the community to develop, expand and improve these utilities for paleogeoscience community.
Last Modified: 10/04/2018
Modified by: Nicholas P Mckay
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