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Observed variations in U.S. frost timing linked to atmospheric circulation patterns
Courtenay Strong1, Gregory J McCabe2
1Department of Atmospheric Sciences, University of Utah, 135 S 1460 E, Salt Lake City, Utah 84112-0110, USA.
Nature Communications
|May 24, 2017
Summary
Atmospheric circulation patterns significantly influence frost timing in the United States, explaining more variability than warming alone. Understanding these patterns is crucial for projecting future growing season lengths.
Area of Science:
- Climatology
- Atmospheric Science
- Agronomy
Background:
- Observed lengthening of the frost-free season in the U.S. over the past century is documented.
- Trends in spring and fall frost timing are linked to hemispheric warming, but circulation anomalies also affect frost timing.
Purpose of the Study:
- To objectively partition the U.S. into regions and identify atmospheric circulations driving frost timing.
- To clarify the relative importance of atmospheric circulation versus warming on frost timing.
Main Methods:
- Objective partitioning of the conterminous United States into four distinct regions.
- Analysis of atmospheric circulation patterns and their correlation with spring and fall frost timing.
Main Results:
- Identified specific atmospheric circulations that account for 25-48% of spring and fall frost timing variability.
- These identified circulations appear responsive to historical warming.
- Circulation patterns explained more frost timing variability than regional or hemispheric temperature indices.
Conclusions:
- Atmospheric circulation plays a more significant role in U.S. frost timing than previously established by temperature indices alone.
- Accurate projections of future growing season length rely on the fidelity of these circulation patterns in global climate models.
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