The Regional Influence of the Arctic Oscillation and Arctic Dipole on the Wintertime Arctic Surface Radiation Budget and Sea Ice Growth

An analysis of 2000-2015 monthly Clouds and the Earth's Radiant Energy System-Energy Balanced and Filled (CERES-EBAF) and Modern-Era Retrospective Analysis for Research and Applications, Version 2 (MERRA2) data reveals statistically significant fall and wintertime relationships between Arctic s...

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Published inGeophysical research letters Vol. 44; no. 9; pp. 4341 - 4350
Main Authors Hegyi, Bradley M., Taylor, Patrick C.
Format Journal Article
LanguageEnglish
Published Langley Research Center American Geophysical Union 16.05.2017
John Wiley & Sons, Inc
Subjects
Anomalies
Arctic Oscillation
Arctic radiation
Arctic sea ice
Atmosphere
Atmospheric temperature
Atmospheric variability
cloud radiative effect
Clouds
Dipoles
Downwelling
Energy
Energy balance
Fluctuations
Flux
large‐scale atmospheric variability
longwave surface fluxes
Meteorological satellites
Ocean-atmosphere interaction
Oceanography
Oscillations
Radiation
Radiation budget
Sea ice
Sea ice growth
Sky
Statistical analysis
Temperature
Terrestrial radiation
Water temperature
Water vapor
winter
PNE, Kara Sea
PNE, Barents Sea
Eurasia
Arctic region
Online AccessGet full text
ISSN0094-8276
1944-8007
DOI10.1002/2017GL073281

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Abstract An analysis of 2000-2015 monthly Clouds and the Earth's Radiant Energy System-Energy Balanced and Filled (CERES-EBAF) and Modern-Era Retrospective Analysis for Research and Applications, Version 2 (MERRA2) data reveals statistically significant fall and wintertime relationships between Arctic surface longwave (LW) radiative flux anomalies and the Arctic Oscillation (AO) and Arctic Dipole (AD). Signifying a substantial regional imprint, a negative AD index corresponds with positive downwelling clear-sky LW flux anomalies (greater than10W m(exp -2)) north of western Eurasia (0 deg E-120 deg E) and reduced sea ice growth in the Barents and Kara Seas in November-February. Conversely, a positive AO index coincides with negative clear-sky LW flux anomalies and minimal sea ice growth change in October-November across the Arctic. Increased (decreased) atmospheric temperature and water vapor coincide with the largest positive (negative) clear-sky flux anomalies. Positive surface LW cloud radiative effect anomalies also accompany the negative AD index in December-February. The results highlight a potential pathway by which Arctic atmospheric variability influences the regional surface radiation budget over areas of Arctic sea ice growth.
AbstractList An analysis of 2000–2015 monthly Clouds and the Earth's Radiant Energy System‐Energy Balanced and Filled (CERES‐EBAF) and Modern‐Era Retrospective Analysis for Research and Applications, Version 2 (MERRA2) data reveals statistically significant fall and wintertime relationships between Arctic surface longwave (LW) radiative flux anomalies and the Arctic Oscillation (AO) and Arctic Dipole (AD). Signifying a substantial regional imprint, a negative AD index corresponds with positive downwelling clear‐sky LW flux anomalies (>10 W m−2) north of western Eurasia (0°E–120°E) and reduced sea ice growth in the Barents and Kara Seas in November–February. Conversely, a positive AO index coincides with negative clear‐sky LW flux anomalies and minimal sea ice growth change in October–November across the Arctic. Increased (decreased) atmospheric temperature and water vapor coincide with the largest positive (negative) clear‐sky flux anomalies. Positive surface LW cloud radiative effect anomalies also accompany the negative AD index in December–February. The results highlight a potential pathway by which Arctic atmospheric variability influences the regional surface radiation budget over areas of Arctic sea ice growth.
An analysis of 2000–2015 monthly Clouds and the Earth's Radiant Energy System‐Energy Balanced and Filled (CERES‐EBAF) and Modern‐Era Retrospective Analysis for Research and Applications, Version 2 (MERRA2) data reveals statistically significant fall and wintertime relationships between Arctic surface longwave (LW) radiative flux anomalies and the Arctic Oscillation (AO) and Arctic Dipole (AD). Signifying a substantial regional imprint, a negative AD index corresponds with positive downwelling clear‐sky LW flux anomalies (>10 W m−2) north of western Eurasia (0°E–120°E) and reduced sea ice growth in the Barents and Kara Seas in November–February. Conversely, a positive AO index coincides with negative clear‐sky LW flux anomalies and minimal sea ice growth change in October–November across the Arctic. Increased (decreased) atmospheric temperature and water vapor coincide with the largest positive (negative) clear‐sky flux anomalies. Positive surface LW cloud radiative effect anomalies also accompany the negative AD index in December–February. The results highlight a potential pathway by which Arctic atmospheric variability influences the regional surface radiation budget over areas of Arctic sea ice growth. Key Points Low‐frequency atmospheric variability in winter projects regionally onto the Arctic surface radiation budget Clear‐sky surface downwelling longwave anomalies associated with the AO and AD driven by near‐surface moisture and temperature changes Reduced November‐February sea ice growth in Barents/Kara Seas associated with negative AD pattern
An analysis of 2000–2015 monthly Clouds and the Earth's Radiant Energy System‐Energy Balanced and Filled (CERES‐EBAF) and Modern‐Era Retrospective Analysis for Research and Applications, Version 2 (MERRA2) data reveals statistically significant fall and wintertime relationships between Arctic surface longwave (LW) radiative flux anomalies and the Arctic Oscillation (AO) and Arctic Dipole (AD). Signifying a substantial regional imprint, a negative AD index corresponds with positive downwelling clear‐sky LW flux anomalies (>10 W m −2 ) north of western Eurasia (0°E–120°E) and reduced sea ice growth in the Barents and Kara Seas in November–February. Conversely, a positive AO index coincides with negative clear‐sky LW flux anomalies and minimal sea ice growth change in October–November across the Arctic. Increased (decreased) atmospheric temperature and water vapor coincide with the largest positive (negative) clear‐sky flux anomalies. Positive surface LW cloud radiative effect anomalies also accompany the negative AD index in December–February. The results highlight a potential pathway by which Arctic atmospheric variability influences the regional surface radiation budget over areas of Arctic sea ice growth. Low‐frequency atmospheric variability in winter projects regionally onto the Arctic surface radiation budget Clear‐sky surface downwelling longwave anomalies associated with the AO and AD driven by near‐surface moisture and temperature changes Reduced November‐February sea ice growth in Barents/Kara Seas associated with negative AD pattern
An analysis of 2000-2015 monthly Clouds and the Earth's Radiant Energy System-Energy Balanced and Filled (CERES-EBAF) and Modern-Era Retrospective Analysis for Research and Applications, Version 2 (MERRA2) data reveals statistically significant fall and wintertime relationships between Arctic surface longwave (LW) radiative flux anomalies and the Arctic Oscillation (AO) and Arctic Dipole (AD). Signifying a substantial regional imprint, a negative AD index corresponds with positive downwelling clear-sky LW flux anomalies (greater than10W m(exp -2)) north of western Eurasia (0 deg E-120 deg E) and reduced sea ice growth in the Barents and Kara Seas in November-February. Conversely, a positive AO index coincides with negative clear-sky LW flux anomalies and minimal sea ice growth change in October-November across the Arctic. Increased (decreased) atmospheric temperature and water vapor coincide with the largest positive (negative) clear-sky flux anomalies. Positive surface LW cloud radiative effect anomalies also accompany the negative AD index in December-February. The results highlight a potential pathway by which Arctic atmospheric variability influences the regional surface radiation budget over areas of Arctic sea ice growth.
Audience PUBLIC
Author Taylor, Patrick C.
Hegyi, Bradley M.
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Snippet An analysis of 2000-2015 monthly Clouds and the Earth's Radiant Energy System-Energy Balanced and Filled (CERES-EBAF) and Modern-Era Retrospective Analysis for...
An analysis of 2000–2015 monthly Clouds and the Earth's Radiant Energy System‐Energy Balanced and Filled (CERES‐EBAF) and Modern‐Era Retrospective Analysis for...
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SubjectTerms Anomalies
Arctic Oscillation
Arctic radiation
Arctic sea ice
Atmosphere
Atmospheric temperature
Atmospheric variability
cloud radiative effect
Clouds
Dipoles
Downwelling
Energy
Energy balance
Fluctuations
Flux
large‐scale atmospheric variability
longwave surface fluxes
Meteorological satellites
Ocean-atmosphere interaction
Oceanography
Oscillations
Radiation
Radiation budget
Sea ice
Sea ice growth
Sky
Statistical analysis
Temperature
Terrestrial radiation
Water temperature
Water vapor
winter
Title The Regional Influence of the Arctic Oscillation and Arctic Dipole on the Wintertime Arctic Surface Radiation Budget and Sea Ice Growth
URI https://ntrs.nasa.gov/citations/20170008763
https://onlinelibrary.wiley.com/doi/abs/10.1002%2F2017GL073281
https://www.proquest.com/docview/1902429489
Volume 44
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