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Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
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In a nonhomogeneous rod made up of steel and brass, restrained at both ends and subjected to a temperature change, several steps are involved in calculating the stress and compressive load. Due to the problem's static indeterminacy, one end support is disconnected, allowing the rod to experience the temperature change freely. Next, an unknown force is applied at the free end, triggering deformations in the rod's steel and brass portions. These deformations are then calculated and added...
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Esophageal Heat Transfer for Patient Temperature Control and Targeted Temperature Management
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Constraints on global temperature target overshoot.

K L Ricke1,2, R J Millar3, D G MacMartin4

  • 1Scripps Institution of Oceanography, UC San Diego, La Jolla, USA. kricke@ucsd.edu.

Scientific Reports
|November 9, 2017
PubMed
Summary
This summary is machine-generated.

Limiting global warming requires rapid energy decarbonization and carbon dioxide removal. The duration of temporary temperature overshoot depends on both, with ambitious strategies needed to keep it under two centuries.

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Area of Science:

  • Climate Science
  • Energy Policy
  • Environmental Science

Background:

  • The Paris Agreement necessitates assessing pathways to limit global warming to 1.5°C or 2°C.
  • Understanding temperature overshoot is crucial for climate policy discussions.

Purpose of the Study:

  • To analyze the impact of energy decarbonization and carbon dioxide removal on temperature overshoot.
  • To explore the relationship between these factors and temperature targets.

Main Methods:

  • Utilized data from the mitigation literature and the IPCC Working Group 3 (WG3) scenario database.
  • Examined global mean temperature implications of various decarbonization and negative emissions technology pathways.

Main Results:

  • The magnitude of temperature overshoot is primarily sensitive to the rate of energy decarbonization.
  • Limiting overshoot duration to under 200 years necessitates ambitious decarbonization and negative emissions technology deployment.

Conclusions:

  • The feasibility of temperature targets depends on aggressive energy sector transformation and carbon removal.
  • Future climate impact assessments must consider both the magnitude and duration of temperature overshoot, especially given uncertainties in negative emissions technologies.