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Multiplexed Isothermal Amplification Based Diagnostic Platform to Detect Zika, Chikungunya, and Dengue 1
Published on: March 13, 2018
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Analyzing climate variations at multiple timescales can guide Zika virus response measures
Ángel G Muñoz1,2,3, Madeleine C Thomson2,4,5, Lisa Goddard2
1Atmospheric and Oceanic Sciences/Geophysical Fluid Dynamics Laboratory, Princeton University, Forrestal Campus. Forrestal Road 201, Princeton, NJ, USA.
Gigascience
|October 8, 2016
Summary
Climate factors, including El Niño and climate change, influenced the 2014-2016 Zika virus (ZIKV) epidemic. Extreme climate anomalies resulted from multiple climate signals, not just El Niño or climate change alone.
Area of Science:
- Environmental Science
- Epidemiology
- Climate Science
Background:
- The 2014-2016 Zika virus (ZIKV) emergence coincided with severe drought and high temperatures, linked to El Niño and climate change.
- Previous studies suggest ZIKV transmission is sensitive to climate seasonality and variability, but quantitative assessments are lacking.
Purpose of the Study:
- To quantitatively assess the climate conditions conducive to the 2014-2016 Zika virus epidemic in Latin America.
- To inform the development of climate-informed prevention and control strategies for ZIKV.
Main Methods:
- Employed a novel timescale-decomposition methodology to analyze climate anomalies.
- Differentiated contributions of El Niño, climate change, and other climate variability (year-to-year, decadal).
Main Results:
- Extreme climate anomalies were driven by a combination of climate signals across multiple timescales.
- Brazilian drought (2013-2015) primarily resulted from year-to-year and decadal variability, with minimal long-term trend contribution.
- Warm temperatures (2014-2015) stemmed from the compound effect of climate change, decadal, and year-to-year variability.
Conclusions:
- ZIKV response strategies in Brazil during the 2015-2016 El Niño event may need revision due to expected rainfall changes (La Niña).
- Sustained warm temperatures are anticipated due to long-term and decadal climate signals, impacting future ZIKV risk.
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