Decadal Variability in Spring Sea Ice Concentration Linked to Summer Temperature and NDVI on the Yukon–Kuskokwim Delta

Author:

Hendricks Amy S.1ORCID,Bhatt Uma S.1,Frost Gerald V.2,Walker Donald A.3,Bieniek Peter A.4,Raynolds Martha K.3,Lader Rick T.4,Epstein Howard E.5,Pinzon Jorge E.6,Tucker Compton J.6,Comiso Josefino C.7

Affiliation:

1. a Department of Atmospheric Sciences, College of Natural Science and Mathematics, Geophysical Institute, University of Alaska Fairbanks, Fairbanks, Alaska

2. b ABR, Inc.–Environmental Research and Services, Fairbanks, Alaska

3. c Institute of Arctic Biology, University of Alaska Fairbanks, Fairbanks, Alaska

4. d International Arctic Research Center, University of Alaska Fairbanks, Fairbanks, Alaska

5. e Department of Environmental Sciences, University of Virginia, Charlottesville, Virginia

6. f Biospheric Science Branch, NASA Goddard Space Flight Center, Greenbelt, Maryland

7. g Cryospheric Sciences Branch, NASA Goddard Space Flight Center, Greenbelt, Maryland

Abstract

Abstract Rapidly warming temperatures in the Arctic are driving increasing tundra vegetation productivity, evidenced in both the satellite derived normalized difference vegetation index (NDVI) imagery and field studies. These trends, however, are not uniformly positive across the circumpolar Arctic. One notable region of negative linear NDVI trends that have persisted over the last 15 years is southwest Alaska’s Yukon–Kuskokwim Delta (YKD). Negative NDVI trends in the YKD region appear inconsistent with our understanding since tundra vegetation is temperature-limited and air temperatures have increased on the YKD. Analysis over a 40-yr record from 1982 to 2021 reveals distinct decadal variability in the NDVI time series, which continues to produce negative linear trends. Similar decadal variability is also evident in summer warmth and 100-km coastal zone spring sea ice concentrations. This suggests that decadal climate variations can dominate the trends of NDVI through their influence on the drivers of tundra vegetation, namely, coastal sea ice concentrations and summer warmth. The relationships among sea ice, summer warmth, and NDVI have changed over the 40-yr record. Seasonality analysis since 1982 shows declining sea ice concentration in spring is followed by trends of increasing temperatures, but weakly declining NDVI during the growing season. An additional key finding is that since early 2010s, the relationships between sea ice concentration and summer warmth, and sea ice concentration and NDVI have strengthened, while the relationship between NDVI and summer warmth has weakened, indicating that temperature may no longer be the primary limiting factor for Arctic tundra vegetation on the YKD. Significance Statement This paper addresses a curiosity of regional Arctic climate change, which is that despite increasing temperatures, spatially and temporally declining trends of vegetation productivity on the Yukon–Kuskokwim Delta appear in satellite data. This study bridges our understanding of Arctic climate relationships at varying scales and informs questions about how these relationships may change in the future.

Funder

National Aeronautics and Space Administration

Publisher

American Meteorological Society

Subject

General Earth and Planetary Sciences

Reference51 articles.

1. Alaska Interagency Coordination Center, 2022: Welcome to the Alaska Interagency Coordination Center. Alaska Interagency Coordination Center, accessed 2 September 2022, https://fire.ak.blm.gov/.

2. Ballinger, T. J., and Coauthors, 2022: Arctic Report Card 2020: Surface air temperature. NOAA, 7 pp., https://doi.org/10.25923/gcw8-2z06.

3. Summer warming explains widespread but not uniform greening in the Arctic tundra biome;Berner, L. T.,2020

4. Circumpolar Arctic tundra vegetation change is linked to sea ice decline;Bhatt, U. S.,2010

5. Changing seasonality of panarctic tundra vegetation in relationship to climatic variables;Bhatt, U. S.,2017

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