Same for the temperature measurements, what part
of the photosphere is the correct solar temperature?
The difference between modeled and observed TSI might be the result of underrepresented weak magnetic fields in the Carrington rotation synoptic charts, an uncertainty in the TSI measurement, or a decline of the global temperature
of the photosphere.
If a band is free of lines, that cooling capacity is unhindered; but if it has important absorption lines, it will be «blocked» = > the same sort
of photosphere questions we have discussed before: a high - altitude photosphere means little power can be transported through that band, whereas an unencumbered band has its photosphere at ground - level.
EGHE, where atmospheric opacity to LWR raises height of topopause, reduces temp
of photosphere, causes temperature rise at surface: this seems like a case of the tail wagging the dog; dare I use the term unphysical.
2) As you say, when more GHG is added, the altitude
of the photosphere rises (I don't see that the tropopause would rise), and its temperature is reduced: so less power must be radiated away.
You say that where the OD = 1 point, which represents the radius
of the photosphere for IR, and as the concentration of CO2 increases, this radius shifts upwards.
That means that CO2 is in a leveraged position (near the top) to influence the altitude
of the photosphere.
The Sun's radius is measured from its center to the edge
of the photosphere.
During partial eclipses most sunlight is blocked by the Moon passing in front of the Sun, but the uncovered parts
of the photosphere have the same surface brightness as during a normal day.
The solar atmosphere is made up
of the photosphere, the chromosphere, a transition region, and the corona.
The solar atmosphere above that consists
of the photosphere, chromosphere, a transition region and the corona.
Therefore, the outer edge
of the photosphere looks dark, an effect called limb darkening that accounts for the clear crisp edge of the sun's surface.
However, the sun's is composed
of the photosphere, the chromosphere and the corona.
Data about the magnetic field
of the photosphere, which is colder and denser than the corona, were collected by the satellite and enabled the researchers to calculate the evolution of the magnetic environment in the corona during this period of time.
Between 1,500 kilometers from the top
of the photosphere and 10,000 kilometers is a region called the «transition zone,» which is where the atoms are accelerated.
Not exact matches
The structures are anchored in the dense
photosphere, the visible surface
of the Sun.
At its closest it will be within 4 million miles
of the roiling solar surface, known as the
photosphere.
To unknot the
photosphere's tangled mats, the corona must release some
of the energy stored there, Caspi says.
Just keeping count
of the number
of spots, for example, led to recognition
of the 11 - year sunspot cycle that waxes from «solar minimum,» when very few spots are seen, to «solar maximum,» when great conglomerations
of planet - size splotches pockmark the
photosphere, or visible surface
of the sun.
The older idea that acoustic waves flowing out
of lower levels heats the corona was abandoned in the 1970s, when the Orbiting Solar Observatory 8 spacecraft did not see such waves in the chromosphere, the layer just above the
photosphere (the apparent «surface»
of the sun in visible light).
«The fact that the outermost region
of the sun's atmosphere is at millions
of degrees while the temperature
of the underlying
photosphere is only 6,000 kelvins (degrees C. above absolute zero) is quite nonintuitive.
A sunspot is a region on the Sun's surface (
photosphere) that is marked by a lower temperature than its surroundings and intense magnetic activity, which inhibits convection, forming areas
of low surface temperature.
Total solar eclipses, seen from Chile on April 16, 1893 (left) and from Mexico on March 7, 1970 (right), reveal the sun's powerful corona, streaming from its
photosphere at temperatures
of more than 1,000,000 degrees F.
It will do this via high - speed (sub-second timescales) spectroscopic and magnetic measurements
of the solar
photosphere, chromosphere and corona.
«White - light flares correspond to the most extreme cases
of this phenomenon, where so much energy is dumped into the chromosphere and corona that the energy propagates downward to the
photosphere, heating it up, and producing the excess brightness that we observe in white light,» according to another
of the authors, Jorge Sánchez Almeida,
of the Instituto de Astrofísica de Canarias (IAC).
The corona is heated to millions
of degrees, yet the lower atmospheric layers like the
photosphere — the visible surface
of the Sun — are only heated to a few thousand degrees.
This result is in very good agreement with observations carried out on the
photosphere and the corona: the formation
of the magnetic rope coincides with changes in sunspots in the region
of the flare and with the emergence
of other structures3.
The Sun's atmosphere is made up
of a number
of layers including the
photosphere, which is the equivalent
of the Sun's surface, and the corona, the outermost region where flares take place.
The difference between the assumed lightsource (stellar disk) and the actual lightsource
of unknown spectrum (
photosphere under the chord) imprints itself onto the transmission spectrum observed.
The mass loading required in this model can be achieved through interaction with the interstellar medium (ISM), the sputtering
of the dwarf atmosphere by auroral currents, a volcanically active orbiting planet or magnetic reconnection in the
photosphere.
In reality, the stellar spectrum does not cancel out in transmission spectroscopy, because the first - order approximation described above confusingly equates two different light sources: the stellar disk (the spectrum
of which is observed before the transit) and the actual light source, which is just a very small fraction
of the stellar disk — the projection
of the transit chord onto the stellar
photosphere (see figure).
Stars are not perfect: in reality, no patch
of the stellar
photosphere has the same exact spectrum as the stellar chord.
It was long thought that objects at the transition region would display
photospheres with patches
of clouds and cloud - free regions.
The temperature
of a star determines its spectral type, because the energy modifies the physical properties
of the plasma in the
photosphere.
Because there is a temperature gradient between the core
of a star and its surface, energy is steadily transported upward through the intervening layers until it is radiated away at the
photosphere.
[17] The star is radiating 1.5 [10] times the Sun's luminosity from its
photosphere at an effective temperature
of 6,149 K. [11]
To see what sunspots looks like using modern instrumentation, here are two images
of the sun's
photosphere, taken by the Solar and Heliospheric Observatory (a joint project
of NASA and the European Space Agency).
Question from the week before: What is the third most common element in the
photosphere of the Sun by weight?
The star's
photosphere, or «surface» as seen in visible light, varies in size as it pulsates from about the diameter
of Mars» orbit around the Sun to that
of the asteroid belt.
The outer atmosphere will expand significantly, and planet Earth will lie within the Sun's
photosphere (the part
of the Sun that is not transparent to light).
To carry out novel investigations based on spectro - polarimetric observations with ground - based and space solar telescopes, with emphasis on the study
of the magnetic field in chromospheric and coronal structures and its coupling with the underlying
photosphere.
The corona can be seen only during solar eclipses because it is millions
of times fainter than the
photosphere.
The part
of the Sun that we see from Earth is called the
photosphere.
The
photosphere is the lowest layer
of the sun's atmosphere, and emits the light we see.
Since the outer gas envelopes
of the stars are in contact (overflowing their Roche lobes), they essentially share a common
photosphere despite having two distinct nuclear - burning cores.
The
photosphere is the lowest region
of the sun's atmosphere and is the region that we can see.
High - dispersion spectroscopy confirmed the presence
of light from a cool stellar
photosphere in the spectrum
of this system.
It extends millions
of kilometers into space and is a million times fainter than the
photosphere.
«The surface
of the sun» typically refers to the
photosphere, at least in lay terms.
As gases churn in the
photosphere, they produce shock waves that heat the surrounding gas and send it piercing through the chromosphere in millions
of tiny spikes
of hot gas called spicules.