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Photoelectron diffraction: from phenomenological demonstration to practical tool
The potential of photoelectron diffraction—exploiting the coherent interference of directly-emitted and elastically scattered components of the photoelectron wavefield emitted from a core level of a surface atom to obtain structural information—was first appreciated in the 1970s. The first demonstrations of the effect were published towards the end of that decade, but the method has now entered the mainstream armoury of surface structure determination. This short review has two objectives: First, to outline the way that the idea emerged and the way this evolved in my own collaboration with Neville Smith and his colleagues at Bell Labs in the early years: Second, to provide some insight into the current state-of-the art in application of (scanned-energy mode) photoelectron diffraction to address two key issue in quantitative surface structure determination, namely, complexity and precision. In this regard a particularly powerful aspect of photoelectron diffraction is its elemental and chemical-state specificity
Fibrin-Mediated Delivery of an Ovarian Follicle Pool in a Mouse Model of Infertility
The cryopreservation and autotransplantation of ovarian tissue is emerging as a powerful approach for preserving fertility. However, for cancer patients, it may not be possible to transplant ovarian tissue due to the risk of re-seeding disease. We investigated strategies for transplantation of individually isolated follicles to minimize the risk of re-introducing cancer cells present within the vasculature of ovarian stroma. Procedures for large-scale isolation of early-stage follicles and their encapsulation into fibrin hydrogels were developed. For in vivo validation studies, mice were ovariectomized and transplanted with encapsulated follicles into the ovarian bursa. A substantial increase in the number of secondary follicles was observed in the graft at 9 days after transplantation, and antral follicles by day 21, demonstrating primordial follicle recruitment into the growing pool. Initially, elevated follicle-stimulating hormone levels declined substantially by day 21, indicating feedback from the graft; presence of corpora lutea showed the graft's capability of restoring hormone cyclicity. Taken together, the transplanted follicles were able to engraft, mature, and restore ovarian function in an infertile mouse. This biomaterial may, thus, provide a platform for follicle transplantation with a low risk of cancer contamination and for developing strategies that preserve fertility for women facing a cancer diagnosis.Peer Reviewedhttps://deepblue.lib.umich.edu/bitstream/2027.42/140230/1/ten.tea.2013.0675.pd
Extended Reconstructed Sea Surface Temperature Version 4 (ERSST.v4): Part II. Parametric and Structural Uncertainty Estimations
Described herein is the parametric and structural uncertainty quantification for the monthly Extended
Reconstructed Sea Surface Temperature (ERSST) version 4 (v4). A Monte Carlo ensemble approach was
adopted to characterize parametric uncertainty, because initial experiments indicate the existence of significant
nonlinear interactions. Globally, the resulting ensemble exhibits a wider uncertainty range before 1900, as well
as an uncertainty maximum around World War II. Changes at smaller spatial scales in many regions, or for
important features such as Niño-3.4 variability, are found to be dominated by particular parameter choices.
Substantial differences in parametric uncertainty estimates are found between ERSST.v4 and the
independently derived Hadley Centre SST version 3 (HadSST3) product. The largest uncertainties are over
the mid and high latitudes in ERSST.v4 but in the tropics in HadSST3. Overall, in comparison with HadSST3,
ERSST.v4 has larger parametric uncertainties at smaller spatial and shorter time scales and smaller parametric
uncertainties at longer time scales, which likely reflects the different sources of uncertainty quantified
in the respective parametric analyses. ERSST.v4 exhibits a stronger globally averaged warming trend than
HadSST3 during the period of 1910–2012, but with a smaller parametric uncertainty. These global-mean trend
estimates and their uncertainties marginally overlap.
Several additional SST datasets are used to infer the structural uncertainty inherent in SST estimates. For the
global mean, the structural uncertainty, estimated as the spread between available SST products, is more often
than not larger than the parametric uncertainty in ERSST.v4. Neither parametric nor structural uncertainties
call into question that on the global-mean level and centennial time scale, SSTs have warmed notably
Applying laboratory thermal desorption data in an interstellar context: sublimation of methanol thin films
Methods by which experimental measurements of thermal desorption can be applied in astrophysical environments have been developed, using the sublimation of solid methanol as an example. The temperature programmed desorption of methanol from graphitic, amorphous silica and polycrystalline gold substrates was compared, with the kinetic parameters of desorption extracted by either a leading edge analysis or by fitting using a stochastic integration method. At low coverages, the desorption shows a substrate-dependent fractional order. However, at higher coverages methanol desorption is zeroth order with kinetic parameters independent of substrate. Using a kinetic model based on the stochastic integration analyses, desorption under astrophysically relevant conditions can be simulated. We find that the chemical and morphological nature of the substrate has relatively little impact on the desorption temperature of solid methanol, and that the substrate independent zeroth-order kinetics can provide a satisfactory model for desorption in astrophysical environments. Uncertainties in the heating rate and the distribution of grain sizes will have the largest influence on the range of desorption temperature. These conclusions are likely to be generally applicable to all species in dust grain ice mantles
Estimation of the spontaneous mutation rate in Heliconius melpomene
This is the final published version. It first appeared at mbe.oxfordjournals.org/content/early/2014/11/03/molbev.msu302.abstract.We estimated the spontaneous mutation rate in Heliconius melpomene by genome sequencing of\ud
a pair of parents and 30 of their offspring, based on the ratio of number of de novo heterozygotes\ud
to the number of callable site-individuals. We detected nine new mutations, each one affecting a\ud
single site in a single offspring. This yields an estimated mutation rate of 2.9 x 10-9 (95%\ud
confidence interval, 1.3 x 10-9 - 5.5 x 10-9), which is similar to recent estimates in Drosophila\ud
melanogaster, the only other insect species in which the mutation rate has been directly estimated.\ud
We infer that recent effective population size of H. melpomene is about 2 million, a substantially\ud
lower value than its census size, suggesting a role for natural selection reducing diversity. We\ud
estimate that H. melpomene diverged from its M?llerian co-mimic H. erato about 6 MYA, a\ud
somewhat later date than estimates based on a local molecular clock.CJ was funded by BBSRC [H01439X/1], JWD was funded by the Herchel Smith Fund and PDK and\ud
RWN were funded by the BBSRC
El Niño, tropical Atlantic warmth, and Atlantic hurricanes over the past 1500 years
Author Posting. © The Author(s), 2009. This is the author's version of the work. It is posted here by permission of Nature Publishing Group for personal use, not for redistribution. The definitive version was published in Nature 460 (2009): 880-883, doi:10.1038/nature08219.Atlantic Tropical Cyclone (TC) activity, as measured by annual storm counts,
reached anomalous levels over the past decade. The short nature of the historical
record and potential issues with its reliability in earlier decades, however, has
prompted an ongoing debate regarding the reality and significance of the recent
rise. Here, we place recent activity in a longer-term context, by comparing two
independent estimates of TC activity over the past 1500 years. The first estimate is
based on a composite of regional sedimentary evidence of landfalling hurricanes,
while the second estimate employs a previously published statistical model of
Atlantic TC activity driven by proxy-reconstructions of past climate changes. Both
approaches yield consistent evidence of a peak in Atlantic TC activity during
Medieval times (around AD 1000) followed by a subsequent lull in activity. The
Medieval peak, which rivals or even exceeds (within uncertainties) recent levels of
activity, results in the statistical model from a ‘perfect storm’ of La Niña-like
climate conditions and relative tropical Atlantic warmth.M.E.M. and Z.Z. acknowledge support from the ATM programme of the National Science Foundation (grant ATM-0542356). J.P.D. acknowledges support from the EAR and OCE programmes of the National Science Foundation (grants EAR-0519118 and OCE-0402746), the Risk Prediction Initiative at the Bermuda Institute for Ocean Sciences, and the Inter-American Institute for Global Change Research
The Pandora multi-algorithm approach to automated pattern recognition of cosmic-ray muon and neutrino events in the MicroBooNE detector
The development and operation of Liquid-Argon Time-Projection Chambers for
neutrino physics has created a need for new approaches to pattern recognition
in order to fully exploit the imaging capabilities offered by this technology.
Whereas the human brain can excel at identifying features in the recorded
events, it is a significant challenge to develop an automated, algorithmic
solution. The Pandora Software Development Kit provides functionality to aid
the design and implementation of pattern-recognition algorithms. It promotes
the use of a multi-algorithm approach to pattern recognition, in which
individual algorithms each address a specific task in a particular topology.
Many tens of algorithms then carefully build up a picture of the event and,
together, provide a robust automated pattern-recognition solution. This paper
describes details of the chain of over one hundred Pandora algorithms and tools
used to reconstruct cosmic-ray muon and neutrino events in the MicroBooNE
detector. Metrics that assess the current pattern-recognition performance are
presented for simulated MicroBooNE events, using a selection of final-state
event topologies.Comment: Preprint to be submitted to The European Physical Journal
Noise Characterization and Filtering in the MicroBooNE Liquid Argon TPC
The low-noise operation of readout electronics in a liquid argon time
projection chamber (LArTPC) is critical to properly extract the distribution of
ionization charge deposited on the wire planes of the TPC, especially for the
induction planes. This paper describes the characteristics and mitigation of
the observed noise in the MicroBooNE detector. The MicroBooNE's single-phase
LArTPC comprises two induction planes and one collection sense wire plane with
a total of 8256 wires. Current induced on each TPC wire is amplified and shaped
by custom low-power, low-noise ASICs immersed in the liquid argon. The
digitization of the signal waveform occurs outside the cryostat. Using data
from the first year of MicroBooNE operations, several excess noise sources in
the TPC were identified and mitigated. The residual equivalent noise charge
(ENC) after noise filtering varies with wire length and is found to be below
400 electrons for the longest wires (4.7 m). The response is consistent with
the cold electronics design expectations and is found to be stable with time
and uniform over the functioning channels. This noise level is significantly
lower than previous experiments utilizing warm front-end electronics.Comment: 36 pages, 20 figure
Measurement of cosmic-ray reconstruction efficiencies in the MicroBooNE LArTPC using a small external cosmic-ray counter
The MicroBooNE detector is a liquid argon time projection chamber at Fermilab
designed to study short-baseline neutrino oscillations and neutrino-argon
interaction cross-section. Due to its location near the surface, a good
understanding of cosmic muons as a source of backgrounds is of fundamental
importance for the experiment. We present a method of using an external 0.5 m
(L) x 0.5 m (W) muon counter stack, installed above the main detector, to
determine the cosmic-ray reconstruction efficiency in MicroBooNE. Data are
acquired with this external muon counter stack placed in three different
positions, corresponding to cosmic rays intersecting different parts of the
detector. The data reconstruction efficiency of tracks in the detector is found
to be , in good agreement with the Monte Carlo reconstruction
efficiency . This analysis represents
a small-scale demonstration of the method that can be used with future data
coming from a recently installed cosmic-ray tagger system, which will be able
to tag of the cosmic rays passing through the MicroBooNE
detector.Comment: 19 pages, 12 figure
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