4,824 research outputs found
On colouring point visibility graphs
In this paper we show that it can be decided in polynomial time whether or
not the visibility graph of a given point set is 4-colourable, and such a
4-colouring, if it exists, can also be constructed in polynomial time. We show
that the problem of deciding whether the visibility graph of a point set is
5-colourable, is NP-complete. We give an example of a point visibility graph
that has chromatic number 6 while its clique number is only 4
Obstacle Numbers of Planar Graphs
Given finitely many connected polygonal obstacles in the
plane and a set of points in general position and not in any obstacle, the
{\em visibility graph} of with obstacles is the (geometric)
graph with vertex set , where two vertices are adjacent if the straight line
segment joining them intersects no obstacle. The obstacle number of a graph
is the smallest integer such that is the visibility graph of a set of
points with obstacles. If is planar, we define the planar obstacle
number of by further requiring that the visibility graph has no crossing
edges (hence that it is a planar geometric drawing of ). In this paper, we
prove that the maximum planar obstacle number of a planar graph of order is
, the maximum being attained (in particular) by maximal bipartite planar
graphs. This displays a significant difference with the standard obstacle
number, as we prove that the obstacle number of every bipartite planar graph
(and more generally in the class PURE-2-DIR of intersection graphs of straight
line segments in two directions) of order at least is .Comment: Appears in the Proceedings of the 25th International Symposium on
Graph Drawing and Network Visualization (GD 2017
Visibility based angular power spectrum estimation in low frequency radio interferometric observations
We present two estimators to quantify the angular power spectrum of the sky
signal directly from the visibilities measured in radio interferometric
observations. This is relevant for both the foregrounds and the cosmological
21-cm signal buried therein. The discussion here is restricted to the Galactic
synchrotron radiation, the most dominant foreground component after point
source removal. Our theoretical analysis is validated using simulations at 150
MHz, mainly for GMRT and also briefly for LOFAR. The Bare Estimator uses
pairwise correlations of the measured visibilities, while the Tapered Gridded
Estimator uses the visibilities after gridding in the uv plane. The former is
very precise, but computationally expensive for large data. The latter has a
lower precision, but takes less computation time which is proportional to the
data volume. The latter also allows tapering of the sky response leading to
sidelobe suppression, an useful ingredient for foreground removal. Both
estimators avoid the positive bias that arises due to the system noise. We
consider amplitude and phase errors of the gain, and the w-term as possible
sources of errors . We find that the estimated angular power spectrum is
exponentially sensitive to the variance of the phase errors but insensitive to
amplitude errors. The statistical uncertainties of the estimators are affected
by both amplitude and phase errors. The w-term does not have a significant
effect at the angular scales of our interest. We propose the Tapered Gridded
Estimator as an effective tool to observationally quantify both foregrounds and
the cosmological 21-cm signal.Comment: 20 pages, 15 figures, 1 table.One typo corrected in Fig.13. Accepted
for publication in MNRA
Reviving sub-TeV lepton doublet Dark Matter
In this work we study the hybrid kind of dark matter(DM) production mechanism
where both thermal and non-thermal contribution at two different epochs set the
DM relic abundance. This hybrid set up in turn shifts the parameter space of DM
in contrast to pure thermal DM scenario. We review such production mechanism in
the context of the lepton doublet dark matter () augmented with
an additional singlet dark scalar (). The neutral component of the dark
doublet can serve as a stable DM candidate and in pure thermal scenario, it is
under-abundant as well as excluded from direct detection constraints due to its
strong gauge interactions in the sub-TeV mass regime. However, in addition to
the thermal contribution, the late time non-thermal DM production from the
decay of the long-lived dark scalar helps to fulfill the deficit in DM
abundance. On the other hand, the strong gauge mediated direct detection
constraint can be evaded with the help of a triplet scalar(with
), resulting a pseudo-Dirac DM. To realize our proposed scenario we impose
a discrete symmetry under which both and are odd
while rest of the fields are even. We find the lepton doublet pseudo-Dirac DM
with mass GeV, compatible with the observed relic density,
direct, indirect, and existing collider search constraints.Comment: 15 page
CMB signature of non-thermal Dark Matter produced from self-interacting dark sector
The basic idea of this work is to achieve the observed relic density of a
non-thermal dark matter(DM) and its connection with Cosmic Microwave Background
(CMB) via additional relativistic degrees of freedom which are simultaneously
generated during the period from a
long-lived dark sector particle. To realize this phenomena we minimally extend
the type-I seesaw scenario with a Dirac fermion singlet() and a complex
scalar singlet () which transform non-trivially under an unbroken
symmetry . being the lightest particle in the dark sector
acts as a stable dark matter candidate while the next to lightest state
operates like a long lived dark scalar particle. The initial density
of can be thermally produced through either self-interacting number
changing processes () within dark sector or the
standard annihilation to SM particles (). The late
time (after neutrino decoupling) non-thermal decay of can produce
dark matter in association with active neutrinos. The presence of extra
relativistic neutrino degrees of freedom at the time of CMB can have a
significant impact on . Thus the precise measurement of
by current PLANCK 2018 collaboration and future
experiments like SPT-3G and CMB-S4 can indirectly probe this non-thermal dark
matter scenario which is otherwise completely secluded due to its tiny coupling
with the standard model.Comment: Accepted for publication in JCA
Performance Evaluation of Open-Ended ELSS Mutual Fund Schemes in India during Recession
This study examined the performance of the open-ended equity linked saving mutual fund schemes (ELSS) in India during the financial distress in 2008-2009. In this study, the month end net asset values of selected equity linked saving mutual fund schemes were considered and the data was obtained from the website of Association of Mutual Funds in India (AMFI). This paper empirically examined the risk-adjusted, selectivity, diversification and market-timing performances of the open-ended (ELSS) mutual fund schemes. Here, Sharpe, Treynor, Jensen and Treynor & Mazuy models were used to measure the above stated performances. It was observed that the Sharpe and Treynor ratios of the open-ended mutual fund schemes (ELSS) were negative during the recession. Similarly, the stock-selection and market-timing performances of the managers were statistically insignificant and finally, the diversification performances of the mutual fund schemes (ELSS) were found to be unsatisfactory. Therefore, it might be concluded that the overall performances of the open-ended mutual fund schemes (ELSS) were very unsatisfactory during the recession.Keywords: Mutual Fund, Performance, Recession, Sharpe model, Treynor mode
Soil Loss Estimation through USLE and MMF Methods in the Lateritic Tracts of Eastern Plateau Fringe of Rajmahal Traps, India
Laterites of Birbhum district are indentified as the ‘low-level laterites’ of ‘Rarh Plain’ of West Bengal and these are very much prone to severe soil erosion (mainly surface and sub-surface water erosion) in the monsoon season (June - September). Laterites and lateritic soils (locally named ‘Kankara’) of Caniozoic upland (adjoining areas of Rampurhat I block, Birbhum and Shikaripara block, Dumka- the study area), are the direct result of monsoonal wet-dry type of morpho-climatic processes and further laterisation of fluvial deposited materials (formation of surface duricrust) which was coming from Rajmahal Hills of eastern Chotanagpur Plateau (Jharkhand) in late Pleistocene. Such type of vermiform laterites is shaped and dissected by numerous gullies and ravines, giving birth of badland topography (locally named ‘Khoai’) of both degradation and aggradation processes. Before the soil conservation practices it is helpful if the assessment of soil erosion can be transformed into a statement of how fast soil is being eroded. The estimation of rate of annual soil loss is required in that case, because we must have to predict soil loss through effective models under a wide range of conditions. In this study the entire assessment is focused on the application Universal Soil Loss Equation (USLE) and Morgan, Morgan and Finney (MMF) methods in the soil loss estimation of sample slope segments, and relative comparison and suitability of both methods in the precise estimation of predicting soil loss.Keywords: Laterite, Gully, Rainsplash, Overland flow, USLE and MM
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