Florida Climate Institute
Join Us •  E-Newsletter Signup    Follow FCI on Facebook  Follow FCI on Twitter  Follow FCI on LinkedIn
Cross-disciplinary climate research in service of society
  • Home
  • About
    • The Issue
    • Executive Board
    • Staff
  • Events
    • Upcoming Events
      • Florida
      • Other
  • Projects
    • All Projects
    • Ecosystems
      • Agriculture
      • Coastal
      • Terrestrial
    • Natural Resources
      • Climate Sciences
      • Water
      • Energy
      • Land
    • Human Resources
      • Human Dimensions
      • Extension
      • Education
    • Working Groups
  • Resources
    • Data Sets
      • Big Rain Events in SE
      • FISH50
      • Regional Downscaling
      • Seasonal Forecasts
      • Visualization Tool
    • Publications
      • All
      • Journal Articles
      • Reports
      • White Papers
    • Presentations
    • Links
    • Environmental Minute
    • Headline News Archive
    • Newsletters
    • FAQs
  • Opportunities
    • Funding
    • Employment
  • Affiliates
    • List All Affiliates
    • Search By Map
    • Join Us / Register
    • Login
  • Contact

Publications

Home | Show All | Simple Search | Advanced Search | Journal Articles | Reports | White Papers
Login
Quick Search:
...
1-2 of 2 records found matching your query:

toggle visibility
Search within Results:
...
Display Options:

Select All    Deselect All << 1 >>
List View
 | 
Citations
 | 
Details
   print
Carlson, A. E., Dutton, A., Long, A. J., & Milne, G. A. (2019). PALeo constraints on SEA level rise (PALSEA): Ice-sheet and sea-level responses to past climate warming. Quaternary Science Reviews, 212, 28–32.
toggle visibility
Abstract: Here we summarize the motivation and issues surrounding the responses of ice sheets and sea level to past climate warming as part of the PALeo constraints on SEA level rise (PALSEA) working group. Papers in this special issue of Quaternary Science Reviews focus on the timescale of glaciations during the late Pliocene, the magnitude of ice-sheet fluctuations and volume leading up to and during the last glacial maximum, the timing and persistence of ice-sheet impacts on deglacial and future relative sea-level change, and relative sea-level change during peak interglacial climate. A more dynamic cryosphere is noted under both late Pliocene and last glacial cycle climate conditions, while relative sea-level changes during the last deglaciation appear to correspond closely with individual ice-sheet deglaciation. Lastly, relative sea-level change during peak interglacial conditions may have fluctuated by as much as a meter, although the sources of such variability (Greenland, Antarctica or elsewhere) remain elusive. (C) 2019 Elsevier Ltd. All rights reserved.
Keywords: LAST GLACIAL MAXIMUM; LAURENTIDE; PLIOCENE; HISTORY; DEGLACIATION; VOLUMES; RETREAT; RECORD; RATES; COAST
Permanent link
 | Save citation:  RTF  PDF  LaTeX
 | Export record:  Atom XML  MODS XML  ODF XML
details   doi
Li, Y., Ji, R., Jenouvrier, S., Jin, M., & Stroeve, J. (2016). Synchronicity between ice retreat and phytoplankton bloom in circum-Antarctic polynyas: Synchronicity of Ice Retreat and Bloom. Geophys. Res. Lett., 43(5), 2086–2093.
toggle visibility
Abstract: Phytoplankton in Antarctic coastal polynyas has a temporally short yet spatially variant growth window constrained by ice cover and day length. Using 18-year satellite measurements (1997-2015) of sea ice and chlorophyll concentrations, we assessed the synchronicity between the spring phytoplankton bloom and light availability, taking into account the ice cover and the incident solar irradiance, for 50 circum-Antarctic coastal polynyas. The synchronicity was strong (i.e., earlier ice-adjusted light onset leads to earlier bloom and vice versa) in most of the western Antarctic polynyas but weak in a majority of the eastern Antarctic polynyas. The west-east asymmetry is related to sea ice production rate: the formation of many eastern Antarctic polynyas is associated with strong katabatic wind and high sea ice production rate, leading to stronger water column mixing that could damp phytoplankton blooms and weaken the synchronicity.
Keywords: phenology; synchronicity; phytoplankton; ice retreat; Antarctic polynya
Permanent link
 | Save citation:  RTF  PDF  LaTeX
 | Export record:  Atom XML  MODS XML  ODF XML
details   doi
Select All    Deselect All << 1 >>
List View
 | 
Citations
 | 
Details
   print

toggle visibility
Save Citations:
Export Records:

Home CQL Search  |  Library Search  |  Show Record  |  Extract Citations Help

logo-fau-2Florida International UniversityFlorida State UniversityUniversity of Central FloridaUniversity of Floridalogo-um-2University of South Florida

The Florida Climate Institute (FCI) is a multi-disciplinary network of national and international research and public organizations, scientists, and individuals concerned with achieving a better understanding of climate variability and change.

Copyright © Florida Climate Institute. All rights reserved.