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A thermodynamic process that occurs at constant volume is called an isochoric process. According to the first law of thermodynamics, heat supplied or removed from the system is partially utilized to perform work and change the internal energy of the system. However, in an isochoric process, the volume remains constant. Hence, the work done by the system is zero. Therefore, the exchange of heat changes the internal energy of the system only. 
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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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An electric field suffers a discontinuity at a surface charge. Similarly, a magnetic field is discontinuous at a surface current. The perpendicular component of a magnetic field is continuous across the interface of two magnetic mediums. In contrast, its parallel component, perpendicular to the current, is discontinuous by the amount equal to the product of the vacuum permeability and the surface current. Like the scalar potential in electrostatics, the vector potential is also continuous...
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The study of external flow is essential for creating structures and objects that interact efficiently and safely with moving fluids, such as air or water. When a body is immersed in a flowing fluid, it experiences two primary forces: drag, which opposes motion along the flow direction, and lift, which acts perpendicular to the flow. The shape, size, and orientation of the object influence these forces.Streamlined and Blunt Bodies in External FlowObjects in fluid flow are classified as...
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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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Related Experiment Video

Updated: Apr 4, 2026

Evolution of Staircase Structures in Diffusive Convection
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Evolution of Staircase Structures in Diffusive Convection

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Arctic circulation regimes.

Andrey Proshutinsky1, Dmitry Dukhovskoy2, Mary-Louise Timmermans3

  • 1Physical Oceanography Department, Woods Hole Oceanographic Institution, Woods Hole, MA, USA aproshutinsky@whoi.edu.

Philosophical Transactions. Series A, Mathematical, Physical, and Engineering Sciences
|September 9, 2015
PubMed
Summary
This summary is machine-generated.

Arctic climate patterns historically alternated between cyclonic and anticyclonic regimes every 5-7 years. Since 1997, an atypical anticyclonic regime has persisted, disrupting decadal variability.

Keywords:
arctic climate variabilitycirculation regimesfreshwater and heat content

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Area of Science:

  • Arctic environmental science
  • Climate dynamics
  • Oceanography

Background:

  • Arctic environmental parameters exhibited decadal variability from 1948-1996.
  • Two primary circulation patterns, cyclonic and anticyclonic, alternated every 5-7 years.
  • These regimes influenced sea-level pressure, atmospheric conditions, ocean currents, and freshwater flux.

Purpose of the Study:

  • To analyze the shift in Arctic circulation patterns since 1997.
  • To investigate the causes and regulatory mechanisms of Arctic circulation regimes.
  • To explore the impact of freshwater flux changes on Arctic environmental conditions and variability.

Main Methods:

  • Analysis of historical environmental parameters (1948-present).
  • Identification and characterization of cyclonic and anticyclonic circulation regimes.
  • Hypothesis development on regime regulation and freshwater flux impacts.

Main Results:

  • A distinct decadal variability in Arctic environmental parameters was observed until 1996.
  • Since 1997, the Arctic has been under a prolonged anticyclonic regime (17 years).
  • Environmental parameters during the recent anticyclonic regime are atypical.

Conclusions:

  • The established decadal variability of Arctic circulation regimes has been interrupted.
  • Changes in freshwater fluxes from the Arctic Ocean and Greenland may be responsible for altering regime dynamics.
  • Further research is needed to understand the long-term implications of these changes.