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Paleo-event data standards for dendrochronology
Elaine Kennedy Sutherland, P. Brewer and W. Gross
Past Global Changes Magazine
25(3)
163
2017
Elaine Kennedy Sutherland1, P. Brewer2 and W. Gross3
Woodland Park, USA, 10-14 September 2017
Extreme environmental events, such as storm winds, landslides, insect infestations, and wildfire, cause loss of life, resources, and human infrastructure. Disaster risk-reduction analysis can be improved with information about past frequency, intensity, and spatial patterns of extreme events. Tree-ring analyses can provide such information: tree rings reflect events as anatomical anomalies or changed growth patterns at an annual- or even sub-annual resolution (Fig. 1). These centuries-long times series of paleo-events are far longer than historical records.
Dendrochronologists embraced information technology in the 1970s and, over time, developed specialized software using data in formatted, plain-text files. Analytical approaches developed in the 80s and 90s for fire-history analysis (Grissino-Mayer 2001) continue to be used and provide a context to analyze other paleo-events; for example, insect infestations (Speer et al. 2010). The early data structures developed for use in these specialty tools became entrenched and continue to be used today, with some awkwardness and significant limitations. They are inadequate to manage event-related tree-ring data that integrate the disciplines of paleoclimatology, ecology, hydrology, and geomorphology.
With PAGES’ support, 15 dendrochronologists1 from five nations attended a workshop addressing PAGES’ Data Stewardship Integrative Activity2. The goal was to highlight the commonalities and differences among event indicators and to develop a general data model for dendrochronological-event data. After discussing the commonalities and differences among indicators, we agreed to utilize and expand the Tree Ring Data Standard, TRiDaS (Jansma et al. 2010) as a data and metadata structure to promote best practices of data stewardship. We concurred that a common data management framework would facilitate analysis without dictating software usage.
We summarized event indicators observable in wood anatomy, chemistry, and size variation, and the metadata necessary to describe them. We developed a preliminary list of event types, indicators, and new metadata for TRiDaS, agreeing to adopt existing, vetted metadata definitions (in particular the Forest Inventory and Analysis - FIA3) rather than developing new ones. We acknowledged that interoperability with NOAA Paleo, the LiPD format, and LinkedEarth data model (McKay and Emile-Geay 2016) is essential. We agreed to contribute to and to expand the LinkedEarth ontology through the "Trees Working Group" and the NOAA WDS-Paleo ontology, to describe paleo-events, provide a catalogue of current practices, and a list of needed analytical and graphical capabilities. Following these agreements we were easily able to develop a list of products, activities, and outreach efforts that can promote the adoption of these data standards.
In closing, participants agreed that there is sufficient need to merit further development of these concepts with a larger and broader international group. We will seek funding to engage the community in collective crowdsourcing and for the scientific effort needed to create the data framework. In adopting common data standards, this effort can serve the needs of land management and disaster risk-reduction analysis to great societal benefit.
links
1http://fhaes.org
2pastglobalchanges.org/science/int-act/data-stewardship
3www.fia.fs.fed.us
affiliations
1USDA Forest Service, Rocky Mountain Research Station, Missoula, USA
2Laboratory of Tree-Ring Research, University of Arizona, Tucson, USA
3NOAA National Centers for Environmental Information's World Data Service for Paleoclimatology, Boulder, USA
contact
Elaine Kennedy Sutherland: esutherlandfs.fed.us
references
McKay NP, Emile-Geay J (2016) Clim Past 12: 1093-1100
Grissino-Mayer H (2001) Tree-Ring Res 57: 115-124
Jansma E et al. (2010) Dendrochronologia 28: 99-130