NOAA/WDS Paleoclimatology - North Iceland Holocene Chironomid-Inferred July Temperatures
This archived Paleoclimatology Study is available from the NOAA National Centers for Environmental Information (NCEI), under the World Data Service (WDS) for Paleoclimatology. The associated NCEI study type is Climate Reconstruction. The data include parameters of climate reconstructions with a geographic location of Iceland, Northern Europe. The time period coverage is from 11181 to 0 in calendar years before present (BP). See metadata information for parameter and study location details. Please cite this study when using the data.
- Cite as: Axford, Y.; Miller, G.H.; Geirsdóttir, A.; Langdon, P.G. (2020-03-24): NOAA/WDS Paleoclimatology - North Iceland Holocene Chironomid-Inferred July Temperatures. [indicate subset used]. NOAA National Centers for Environmental Information. https://doi.org/10.25921/hbeq-my66. Accessed [date].
- Please refer to Credit tab for full citation information.
- doi:10.25921/hbeq-my66
- noaa-recon-29332
- NCEI DSI 1200_02
- NCEI DSI 1200_01
noaa-recon-29332
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Distributor | NOAA National Centers for Environmental Information
ncei.info@noaa.gov |
Dataset Point of Contact | NOAA National Centers for Environmental Information
ncei.info@noaa.gov |
Dataset Point of Contact | Data Center Contact
NOAA World Data Service for Paleoclimatology 828-271-4800 paleo@noaa.gov |
Coverage Description | Date Range: 11181 cal yr BP to 0 cal yr BP; |
Time Period | -9231 to 1950 |
Spatial Bounding Box Coordinates |
N: 66.24098
S: 66.05945
E: -15.8076
W: -20.38025
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Data Presentation Form | Digital table - digital representation of facts or figures systematically displayed, especially in columns
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Dataset Progress Status | Complete - production of the data has been completed |
Data Update Frequency | Data update frequency not available |
Supplemental Information |
STUDY NOTES: Chironomid-inferred July temperatures for 3 north Iceland lakes for the past 11,100 years
ABSTRACT SUPPLIED BY ORIGINATOR: The Holocene temperature history of Iceland is not well known, despite Iceland's climatically strategic location at the intersection of major surface currents in the high-latitude North Atlantic. Existing terrestrial records reveal spatially heterogeneous changes in Iceland's glacier extent, vegetation cover, and climate over the Holocene, but these records are temporally discontinuous and mostly qualitative. This paper presents the first quantitative estimates of temperatures throughout the entire Holocene on Iceland. Mean July temperatures are inferred based upon subfossil midge (Chironomidae) assemblages from three coastal lakes in northern Iceland. Midge data from each of the three lakes indicate broadly similar temperature trends, and suggest that the North Icelandic coast experienced relatively cool early Holocene summers and gradual warming throughout the Holocene until after 3 ka. This contrasts with many sites on Iceland and around the high-latitude Northern Hemisphere that experienced an early to mid-Holocene "thermal maximum" in response to enhanced summer insolation forcing. Our results suggest a heightened temperature gradient across Iceland in the early Holocene, with suppressed terrestrial temperatures along the northern coastal fringe, possibly as a result of sea surface conditions on the North Iceland shelf. |
Purpose | Records of past temperature, precipitation, and other climate variables derived from paleoclimate proxies. Parameter keywords describe what was measured in this data set. Additional summary information can be found in the abstracts of papers listed in the data set citations. |
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Theme keywords | Global Change Master Directory (GCMD) Science Keywords
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Data Center keywords | Global Change Master Directory (GCMD) Data Center Keywords
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Last Modified: 2024-01-19
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