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Related Concept Videos

Global Climate Change01:50

Global Climate Change

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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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Temperature Dependent Deformation01:12

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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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Isothermal Processes01:21

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A thermodynamic process that occurs at constant temperature is called an isothermal process. Heat slowly flows into the system or out of the system to maintain thermal equilibrium. Processes involving phase changes like water evaporation into steam or freezing water into ice at a constant temperature are examples of Isothermal Processes.
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The spontaneity of a process depends upon the temperature of the system. Phase transitions, for example, will proceed spontaneously in one direction or the other depending upon the temperature of the substance in question. Likewise, some chemical reactions can also exhibit temperature-dependent spontaneities. To illustrate this concept, the equation relating free energy change to the enthalpy and entropy changes for the process is considered:
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Updated: Aug 4, 2025

Using Generative Art to Convey Past and Future Climate Transitions
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Future Indian Ocean warming patterns.

Sahil Sharma1,2, Kyung-Ja Ha3,4,5, Ryohei Yamaguchi6

  • 1Center for Climate Physics, Institute of Basic Science, Busan, South Korea.

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Summary
This summary is machine-generated.

Future Indian Ocean warming is uneven, with hotspots in the Arabian Sea and southeastern Indian Ocean. This study reveals the distinct physical drivers behind these regional warming patterns.

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Area of Science:

  • Climate Science
  • Oceanography
  • Atmospheric Science

Background:

  • Coupled general circulation models project non-uniform Indian Ocean warming.
  • Warming hotspots are identified in the Arabian Sea (AS) and southeastern Indian Ocean (SEIO).
  • The physical drivers of this non-uniform warming remain poorly understood.

Purpose of the Study:

  • To elucidate the causes of non-uniform Indian Ocean warming.
  • To investigate the role of air-sea interactions in regional warming patterns.

Main Methods:

  • Utilizing large ensemble simulations from the Community Earth System Model 2.
  • Analyzing air-sea interactions and their impact on ocean heat transport and atmospheric circulation.

Main Results:

  • Negative air-sea interactions in the Eastern Indian Ocean weaken the zonal sea surface temperature gradient.
  • This leads to a slowdown of the Indian Ocean Walker circulation and southeasterly wind anomalies over the AS.
  • Anomalous northward ocean heat transport, reduced evaporative cooling, and weakened vertical mixing enhance AS warming.
  • Reduced low-cloud cover in the SEIO increases shortwave radiation, contributing to SEIO warming.

Conclusions:

  • Regional air-sea interactions are critical drivers of non-uniform Indian Ocean warming.
  • These regional changes have implications for large-scale tropical atmospheric circulation.
  • The findings highlight the interconnectedness of ocean and atmospheric systems with broad societal and ecological impacts.