31,933 research outputs found
Empirical Constraints on Proton and Electron Heating in the Fast Solar Wind
We analyze measured proton and electron temperatures in the high-speed solar
wind in order to calculate the separate rates of heat deposition for protons
and electrons. When comparing with other regions of the heliosphere, the fast
solar wind has the lowest density and the least frequent Coulomb collisions.
This makes the fast wind an optimal testing ground for studies of collisionless
kinetic processes associated with the dissipation of plasma turbulence. Data
from the Helios and Ulysses plasma instruments were collected to determine mean
radial trends in the temperatures and the electron heat conduction flux between
0.29 and 5.4 AU. The derived heating rates apply specifically for these mean
plasma properties and not for the full range of measured values around the
mean. We found that the protons receive about 60% of the total plasma heating
in the inner heliosphere, and that this fraction increases to approximately 80%
by the orbit of Jupiter. A major factor affecting the uncertainty in this
fraction is the uncertainty in the measured radial gradient of the electron
heat conduction flux. The empirically derived partitioning of heat between
protons and electrons is in rough agreement with theoretical predictions from a
model of linear Vlasov wave damping. For a modeled power spectrum consisting
only of Alfvenic fluctuations, the best agreement was found for a distribution
of wavenumber vectors that evolves toward isotropy as distance increases.Comment: 11 pages (emulateapj style), 5 figures, ApJ, in pres
Polarimetric Imaging of the Massive Black Hole at the Galactic Center
The radio source Sgr A* in the Galactic center emits a polarized spectrum at
millimeter and sub-millimeter wavelengths that is strongly suggestive of
relativistic disk accretion onto a massive black hole. We use the
well-constrained mass of Sgr A* and a magnetohydrodynamic model of the
accretion flow to match both the total flux and polarization from this object.
Our results demonstrate explicitly that the shift in the position angle of the
polarization vector, seen at wavelengths near the peak of the mm to sub-mm
emission from this source, is a signal of relativistic accretion flow in a
strong gravitational field. We provide maps of the polarized emission to
illustrate how the images of polarized intensity from the vicinity of the black
hole would appear in upcoming observations with very long baseline radio
interferometers (VLBI). Our results suggest that near-term VLBI observations
will be able to directly image the polarized Keplerian portion of the flow near
the horizon of the black hole.Comment: 12 pages, 2 figures, Accepted for publciation in ApJ Letter
Sugar additives for MALDI matrices improve signal allowing the smallest nucleotide change (A:T) in a DNA sequence to be resolved
Sample preparation for matrix-assisted laser desorption/ionization (MALDI) mass spectrometry (MS) of DNA is critical for obtaining high quality mass spectra. Sample impurity, solvent content, substrate surface and environmental conditions (temperature and humidity) all affect the rate of matrix–analyte co-crystallization. As a result, laser fluence threshold for desorption/ionization varies from spot to spot. When using 3-hydroxypicolinic acid (3-HPA) as the matrix, laser fluence higher than the threshold value reduces mass resolution in time-of-flight (TOF) MS as the excess energy transferred to DNA causes metastable decay. This can be overcome by either searching for ‘hot’ spots or adjusting the laser fluence. However, both solutions may require a significant amount of operator manipulation and are not ideal for automatic measurements. We have added various sugars for crystallization with the matrix to minimize the transfer of excess laser energy to DNA molecules. Fructose and fucose were found to be the most effective matrix additives. Using these additives, mass resolution for DNA molecules does not show noticeable deterioration as laser energy increases. Improved sample preparation is important for the detection of single nucleotide polymorphisms (SNPs) using primer extension with a single nucleotide. During automatic data acquisition it is difficult to routinely detect heterozygous A/T mutations, which requires resolving a mass difference of 9 Da, unless a sugar is added during crystallization
Pacific Ocean Forcing and Atmospheric Variability are the Dominant Causes of Spatially Widespread Droughts in the Contiguous United States
The contributions of oceanic and atmospheric variability to spatially widespread summer droughts in the contiguous United States (hereafter, pan-CONUS droughts) are investigated using 16-member ensembles of the Community Climate Model version 3 (CCM3) forced with observed sea surface temperatures (SSTs) from 1856 to 2012. The employed SST forcing fields are either (i) global or restricted to the (ii) tropical Pacific or (iii) tropical Atlantic to isolate the impacts of these two ocean regions on pan-CONUS droughts. Model results show that SST forcing of pan-CONUS droughts originates almost entirely from the tropical Pacific because of atmospheric highs from the northern Pacific to eastern North America established by La Nia conditions, with little contribution from the tropical Atlantic. Notably, in all three model configurations, internal atmospheric variability influences pan-CONUS drought occurrence by as much or more than the ocean forcing and can alone cause pan-CONUS droughts by establishing a dominant high centered over the US montane West. Similar results are found for the Community Atmosphere Model version 5 (CAM5). Model results are compared to the observational record, which supports model-inferred contributions to pan-CONUS droughts from La Nias and internal atmospheric variability. While there may be an additional association with warm Atlantic SSTs in the observational record, this association is ambiguous due to the limited number of observed pan-CONUS. The ambiguity thus opens the possibility that the observational results are limited by sampling over the 20th-century and not at odds with the suggested dominance of Pacific Ocean forcing in the model ensembles
Asymptotic theory for a Leidenfrost drop on a liquid pool
Droplets can be levitated by their own vapour when placed onto a superheated
plate (the Leidenfrost effect). It is less known that the Leidenfrost effect
can likewise be observed over a liquid pool (superheated with respect to the
drop), which is the study case here. Emphasis is placed on an asymptotic
analysis in the limit of small evaporation numbers, which proves to be a
realistic one indeed for not so small drops. The global shapes are found to
resemble "superhydrophobic drops" that follow from the equilibrium between
capillarity and gravity. However, the morphology of the thin vapour layer
between the drop and the pool is very different from that of classical
Leidenfrost drops over a flat rigid substrate, and exhibits different scaling
laws. We determine analytical expressions for the vapour thickness as a
function of temperature and material properties, which are confirmed by
numerical solutions. Surprisingly, we show that deformability of the pool
suppresses the chimney instability of Leidenfrost drops
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