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Climate Change: An Inter-disciplinary Approach to Problem Solving��Internal Variability and Temperature

Richard B. Rood

rbrood@umich.edu

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Winter 2021

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GISS Temperature 2002

1997-98 El Niño

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GISS Temperature 2018

1997-98 El Niño

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January 2011 Temperature Anomalies

Eastern Pacific

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January 2011 Temperature Anomalies

Polar – Middle Latitude Variability

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Winter 2014

  • It was very cold in Michigan in Winter 2014.

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Global Map January 2014 Temperature Anomaly

Polar – Middle Latitude Variability

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January 2014 in Perspective

  • U.S.: 53rd coolest, 5th driest
  • Global 4th Warmest

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January 2014: Global Temperature

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What is the consequence of the averaging period?

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GISS Temperature with 1981 - Base

Polar – Middle Latitude Variability

- 6.8 8.3

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GISS Temperature with 1951 - Base

Polar – Middle Latitude Variability

- 4.8 11.2

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GISS Temperature with 1951 - Base

2 degrees warmer compared to 1981 base

- 4.8 11.2

3 degrees warmer compared to 1981 base

Does not appear as cold compared to 1981 base

Appears as warmer compared to 1981 base

Global anomaly nearly 0.5 degrees C higher compared to a 1981 base

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GISS Temperature with 1951 - Base

2 degrees warmer compared to 1981 base

- 4.8 11.2

3 degrees warmer compared to 1981 base

A worrisome cold anomaly in North Atlantic

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Role of El Niño (again)

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Global Map January 2014 Temperature Anomaly

Eastern Pacific

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Eastern Pacific

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Eastern Pacific

A worrisome cold anomaly in North Atlantic

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El Niño – La Niña

El Nino

La Nina

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Pacific Decadal Oscillation in Temperature Record

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Dynamic variability in the temperature record

  • A science-based analysis of the temperature record requires consideration of causes of variability. Can we explain some of the noise? Often, yes.
  • We have in this lecture not considered volcanoes, which are, often, quite important.
  • After we consider all of the causes of variability we can identify and quantify, there remains unexplained variability.
    • Randomness? Irreducible uncertainty?
    • Demand for further investigation.

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