Climate drivers of Arctic tundra variability and change using an indicators framework
Open Access
- 15 February 2021
- journal article
- research article
- Published by IOP Publishing in Environmental Research Letters
- Vol. 16 (5), 055019
- https://doi.org/10.1088/1748-9326/abe676
Abstract
This study applies an indicators framework to investigate climate drivers of tundra vegetation trends and variability over the 1982–2019 period. Previously known indicators relevant for tundra productivity (summer warmth index, coastal spring sea-ice area, coastal summer open-water) and three additional indicators (continentality, summer precipitation, and the Arctic Dipole: second mode of sea level pressure variability) are analyzed with maximum annual Normalized Difference Vegetation Index (MaxNDVI) and the sum of summer bi-weekly (time-integrated) NDVI (TI-NDVI) from the Advanced Very High Resolution Radiometer (AVHRR) time-series. Climatological mean, trends, and correlations between variables are presented. Changes in sea ice continue to drive variations in the other indicators. As spring sea ice has decreased, summer open water, summer warmth, MaxNDVI, and TI-NDVI have increased. However, the initial very strong upward trends in previous studies for MaxNDVI and TI-NDVI are weakening and becoming spatially and temporally more variable as the ice retreats from the coastal areas. TI-NDVI has declined over the last decade particularly over High Arctic regions and southwest Alaska. The Continentality Index (maximum minus minimum monthly temperatures) is decreasing across the tundra, more so over North America than Eurasia. The relationship has weakened between sea-ice and summer warmth index and TI-NDVI, as the maritime influence of open water has increased along with total precipitation. The winter Arctic Dipole is correlated in Eurasia with spring sea ice, summer open water, MaxNDVI, TI-NDVI, the continentality index and total summer precipitation. This winter connection to tundra emphasizes the role of sea ice in driving the summer indicators. The winter (DJF) Arctic Dipole drives sea ice variations which in turn shape summer open water, the atmospheric summer warmth index and NDVI anomalies. The winter and spring indicators represent potential predictors of tundra vegetation productivity a season or two in advance of the growing season.Funding Information
- Climate Program Office (NA17OAR4310160)
- Office of Polar Programs (1263854)
- National Aeronautics and Space Administration (NA17OAR4310160)
This publication has 50 references indexed in Scilit:
- Winter warming events damage sub‐Arctic vegetation: consistent evidence from an experimental manipulation and a natural eventJournal of Ecology, 2009
- Dipole Anomaly in the Winter Arctic Atmosphere and Its Association with Sea Ice MotionJournal of Climate, 2006
- Static mass-balance sensitivity of Arctic glaciers and ice caps using a degree-day approachAnnals of Glaciology, 2005
- Greening of arctic Alaska, 1981–2001Geophysical Research Letters, 2003
- Arctic oscillation and Arctic sea‐ice oscillationGeophysical Research Letters, 2000
- Statistical significance of trends and trend differences in layer‐average atmospheric temperature time seriesJournal of Geophysical Research: Atmospheres, 2000
- The Arctic oscillation signature in the wintertime geopotential height and temperature fieldsGeophysical Research Letters, 1998
- Increased plant growth in the northern high latitudes from 1981 to 1991Nature, 1997
- Satellite remote sensing of primary productionInternational Journal of Remote Sensing, 1986
- Red and photographic infrared linear combinations for monitoring vegetationRemote Sensing of Environment, 1979