This paper presents data from the BIMA interferometer showing spatially resolved absorption spectra of the gravitationally lensed quasar PKS 1830-211. High-resolution (1.2 km s) spectra were taken in two spectral windows centered on the redshifted frequencies of the HCO(2 ← 1) and HCN(2 ← 1) molecular transitions. There is no molecular absorption in the northeast image but the southwest image r...

A network of 25 lightning detection sensors (LDS) has been established by the National Remote Sensing Centre (NRSC), Indian Space Research Organization (ISRO). At present, are located in northeast, east coastal, central, and southern locations India under this network. Geolocation occurrences is estimated using time arrival algorithm. These observations compared well with Institute Tropical Met...

In this paper we present an experimental analysis of several modulation formats (pulse amplitude (PAM-2), quaternary pulse (PAM-4) and electrical duobinary (EDB)) for passive optical network (PON) applications at 25 Gbps bit rate in a C-band 10G-class directly modulated lasers (DML) avalanche photodiode (APD) intensity direct detection (IM-DD) system over single mode fiber (SMF) up to km, optim...

This study presents a plan for seismic monitoring of a region around a potential nuclear power plant. Seismic monitoring is needed to evaluate seismic risk. The International Atomic Energy Agency has set guidelines on seismic hazard evaluation and monitoring of such areas. According to these guidelines, we have made a plan for a local network of seismic stations to collect data for seismic sour...

Copyright © 2016, Infection, Epidemiology and Medicine; Tarbiat Modares University. This is an open-access article distributed under the terms of the Creative Commons Attribution-NonCommercial 4.0 International License, which permits copy and redistribute the material just in noncommercial usages, provided the original work is properly cited Study the Association of Accessory Gene Regulator Typ...

The 2008 Wells earthquake occurred on a northeast-striking, southeast-dipping fault that is clearly delineated by the aftershock swarm to a depth of 10-12 km below sea level. However, Cenozoic rocks and structures around Wells primarily record east-west extension along northto north-northeast-striking, west-dipping normal faults that formed during the middle Miocene. These faults are responsibl...