Related Experiment Video
Updated: Dec 27, 2025

09:17
Experimental Investigation of the Flow Structure over a Delta Wing Via Flow Visualization Methods
Published on: April 23, 2018
11.1K
Apparent and Intrinsic Evolution of Active Region Upflows
Deborah Baker1, Miho Janvier2, Pascal Démoulin3
11Mullard Space Science Laboratory, University College London, Holmbury, St. Mary, Dorking, Surrey, KT22 9XF UK.
Summary
Solar rotation influences observed coronal plasma upflows, with actual evolution depending on active region activity. Upflows often appear in pairs, suggesting non-local driving mechanisms like magnetic reconnection.
Area of Science:
- Solar Physics
- Plasma Physics
- Heliophysics
Background:
- Analysis of Fe xii coronal plasma upflows from active regions (ARs) crossing the solar disk.
- Utilizes data from the Hinode Extreme Ultraviolet Imaging Spectrometer (EIS).
Purpose of the Study:
- To analyze the evolution of Fe xii coronal plasma upflows from active region edges.
- To determine the impact of solar rotation and intrinsic activity on observed upflow evolution.
- To constrain the driving mechanisms of these upflows.
Main Methods:
- Observation of ten active regions (ARs) using Hinode/EIS as they transit the solar disk.
- Analysis of Doppler velocities and line widths of Fe xii spectral lines.
- Estimation of unprojected upflow velocity and inclination using projection effects from solar rotation.
Main Results:
- Observed long-term evolution of upflows is largely due to solar rotation, altering the viewpoint of stationary flows.
- Estimated unprojected upflow velocities fan away from AR cores (40° to vertical for following polarity; -29° to 28° for leading polarity).
- Intrinsic evolution of upflows, dependent on AR activity, is also identified.
- Line widths correlate with Doppler velocities only in ARs with very high velocities.
- Upflows frequently occur in pairs or multiple pairs, indicating a non-local driving mechanism.
Conclusions:
- Solar rotation significantly influences the apparent evolution of coronal upflows.
- Intrinsic AR activity also drives changes in upflow behavior.
- The common occurrence of paired upflows supports models involving reconnection along quasi-separatrix layers, rather than local mechanisms.
Related Concept Videos
Irrotational Flow
848
Irrotational flow is characterized by fluid motion where particles do not rotate around their axes, resulting in zero vorticity. For a flow to be irrotational, the curl of the velocity field must be zero. This imposes specific conditions on velocity gradients. For instance, to maintain zero rotation about the z-axis, the gradient condition:
848
General External Flow Characteristics
473
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...
473
Rapidly Varying Flow
348
Rapidly varying flow (RVF) in open channels is characterized by abrupt changes in flow depth over a short distance, with the rate of depth change relative to distance often approaching unity. These flows are inherently complex due to their transient and multi-dimensional nature, making exact analysis difficult. However, approximate solutions using simplified models provide valuable insights into their behavior.Key Features of Rapidly Varying FlowRVF is commonly observed in scenarios involving...
348
Gradually Varying Flow
335
Gradually varying flow (GVF) in open channels describes situations where water depth changes slowly along the channel due to factors like non-uniform bed slope, channel shape variations, or obstructions. This flow type occurs when the depth adjusts gradually to balance gravitational forces, shear forces, and energy requirements, resulting in a low rate of depth change.Characteristics of Gradually Varying FlowGVF is commonly observed in natural streams, rivers, and canals, where flow depth...
335
Couette Flow
802
Couette flow represents the flow of fluid between two parallel plates, with one plate fixed and the other moving with a constant velocity. This configuration allows for a simplified analysis using the Navier-Stokes equations, which govern fluid motion under conditions of viscosity and incompressibility. For Couette flow, the assumptions include a steady, laminar, incompressible flow with a zero-pressure gradient in the flow direction. This flow type is beneficial for understanding shear-driven...
802
Laminar and Turbulent Flow
10.4K
Fluid dynamics is the study of fluids in motion. Velocity vectors are often used to illustrate fluid motion in applications like meteorology. For example, wind—the fluid motion of air in the atmosphere—can be represented by vectors indicating the speed and direction of the wind at any given point on a map. Another method for representing fluid motion is a streamline. A streamline represents the path of a small volume of fluid as it flows. When the flow pattern changes with time, the...
10.4K

