Search For High Energy Neutrino Induced Cascades With The Amanda-b10 Detector

The Antarctic Muon And Neutrino Detector Array, A<smcap>MANDA</smcap>, is a Cherenkov detector deployed deep in the ice cap at the South Pole. Charged particles traveling faster than the speed of light in ice produce Cherenkov radiation that is detected by Photo-Multiplier Tubes. Using t...

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Main Authors: Toboada-Fermin, I J, Cowen, D F
Language:English
Published: Pennsylvania Univ. 2002
Subjects:
Online Access:http://cds.cern.ch/record/608921
id ftcern:oai:cds.cern.ch:608921
record_format openpolar
spelling ftcern:oai:cds.cern.ch:608921 2023-05-15T13:53:09+02:00 Search For High Energy Neutrino Induced Cascades With The Amanda-b10 Detector Toboada-Fermin, I J Cowen, D F 2002 http://cds.cern.ch/record/608921 eng eng Pennsylvania Univ. http://cds.cern.ch/record/608921 oai:cds.cern.ch:608921 Particle Physics 2002 ftcern 2018-07-28T05:54:54Z The Antarctic Muon And Neutrino Detector Array, A<smcap>MANDA</smcap>, is a Cherenkov detector deployed deep in the ice cap at the South Pole. Charged particles traveling faster than the speed of light in ice produce Cherenkov radiation that is detected by Photo-Multiplier Tubes. Using the information obtained by the Photo- Multiplier Tubes, the physical characteristics, such as direction and energy, can be reconstructed. High energy neutrinos of all flavors can produce particle cascades when interacting with matter. In ice, cascades are typically a few meters long, much smaller than the dimensions of A<smcap>MANDA</smcap>. Electron neutrinos produce cascades via both the charged and neutral current interactions. Muon and tau neutrinos produce cascades via the neutral current interaction. Isolated cascades are also produced by tau neutrinos via charged current interactions, because the resulting tau, at energies below a few hundred TeV, will travel only a few meters before decaying. Advantages of the cascade channel, compared to neutrino induced muons are better energy resolution and an order of magnitude lower background from atmospheric neutrinos when searching for extra terrestrial neutrinos. Data collected in 1997 were searched for high energy neutrino induced cascades. A total of 1.18 × 10 9 events were recorded for an effective live-time of 130.1 days. The overwhelming majority of the events recorded were produced by down-going cosmic-ray induced muons. Bright muon energy losses are the main background when searching for high energy extra- terrestrial neutrino induced cascades. The sensitivity of the detector to cascades has been studied using in-situ light sources. No evidence for the existence of a diffuse flux of high energy neutrinos has been found. Limits have been set for fluxes following an E −2 power law spectrum. For <math> <f> <g>n</g> e + <g>n</g> &d1; e </f> </math> the limit is<display-math> <fd> <fl><g>F</g>E 2 <<rm>5.7-7.1×10 - 6 </rm><hsp sp='0.212'><rm>G<mit>eV</mit></rm>˙s <rm>-1 </rm> ˙sr <rm>-2</rm> <hsp sp='1.000'><hsp sp='0.212'> <rm>90%C.<mit>L<rm>.</rm></mit></rm></fl> </fd> </display-math>For <math> <f> <g>n</g> e + <g>n</g> &d1; e +<g>n</g> <g>m</g> + <g>n</g> &d1; <g>m</g> +<g>n</g> <g>t</g> + <g>n</g> &d1; <g>t</g> </f> </math> the limit is<display-math> <fd> <fl><g>F</g>E <rm>2</rm> <8.5- 10.5×10 - 6 <hsp sp='0.212'><rm>G<mit>eV</mit></rm>˙s <rm> -1</rm> ˙sr <rm>-2</rm> <hsp sp='1.000'><rm> 90%C.</rm><mit>L<rm>.</rm></mit></fl> </fd> </display-math>For both cases the limits are shown with and without the effect of systematic errors. The flux limits were obtained for neutrino energies between 5 TeV and 300 TeV. The effective detector volume has also been calculated for every neutrino flavor, allowing the calculation of fluxes for any neutrino flux model. Other/Unknown Material Antarc* Antarctic Ice cap South pole South pole CERN Document Server (CDS) Antarctic South Pole The Antarctic
institution Open Polar
collection CERN Document Server (CDS)
op_collection_id ftcern
language English
topic Particle Physics
spellingShingle Particle Physics
Toboada-Fermin, I J
Cowen, D F
Search For High Energy Neutrino Induced Cascades With The Amanda-b10 Detector
topic_facet Particle Physics
description The Antarctic Muon And Neutrino Detector Array, A<smcap>MANDA</smcap>, is a Cherenkov detector deployed deep in the ice cap at the South Pole. Charged particles traveling faster than the speed of light in ice produce Cherenkov radiation that is detected by Photo-Multiplier Tubes. Using the information obtained by the Photo- Multiplier Tubes, the physical characteristics, such as direction and energy, can be reconstructed. High energy neutrinos of all flavors can produce particle cascades when interacting with matter. In ice, cascades are typically a few meters long, much smaller than the dimensions of A<smcap>MANDA</smcap>. Electron neutrinos produce cascades via both the charged and neutral current interactions. Muon and tau neutrinos produce cascades via the neutral current interaction. Isolated cascades are also produced by tau neutrinos via charged current interactions, because the resulting tau, at energies below a few hundred TeV, will travel only a few meters before decaying. Advantages of the cascade channel, compared to neutrino induced muons are better energy resolution and an order of magnitude lower background from atmospheric neutrinos when searching for extra terrestrial neutrinos. Data collected in 1997 were searched for high energy neutrino induced cascades. A total of 1.18 × 10 9 events were recorded for an effective live-time of 130.1 days. The overwhelming majority of the events recorded were produced by down-going cosmic-ray induced muons. Bright muon energy losses are the main background when searching for high energy extra- terrestrial neutrino induced cascades. The sensitivity of the detector to cascades has been studied using in-situ light sources. No evidence for the existence of a diffuse flux of high energy neutrinos has been found. Limits have been set for fluxes following an E −2 power law spectrum. For <math> <f> <g>n</g> e + <g>n</g> &d1; e </f> </math> the limit is<display-math> <fd> <fl><g>F</g>E 2 <<rm>5.7-7.1×10 - 6 </rm><hsp sp='0.212'><rm>G<mit>eV</mit></rm>˙s <rm>-1 </rm> ˙sr <rm>-2</rm> <hsp sp='1.000'><hsp sp='0.212'> <rm>90%C.<mit>L<rm>.</rm></mit></rm></fl> </fd> </display-math>For <math> <f> <g>n</g> e + <g>n</g> &d1; e +<g>n</g> <g>m</g> + <g>n</g> &d1; <g>m</g> +<g>n</g> <g>t</g> + <g>n</g> &d1; <g>t</g> </f> </math> the limit is<display-math> <fd> <fl><g>F</g>E <rm>2</rm> <8.5- 10.5×10 - 6 <hsp sp='0.212'><rm>G<mit>eV</mit></rm>˙s <rm> -1</rm> ˙sr <rm>-2</rm> <hsp sp='1.000'><rm> 90%C.</rm><mit>L<rm>.</rm></mit></fl> </fd> </display-math>For both cases the limits are shown with and without the effect of systematic errors. The flux limits were obtained for neutrino energies between 5 TeV and 300 TeV. The effective detector volume has also been calculated for every neutrino flavor, allowing the calculation of fluxes for any neutrino flux model.
author Toboada-Fermin, I J
Cowen, D F
author_facet Toboada-Fermin, I J
Cowen, D F
author_sort Toboada-Fermin, I J
title Search For High Energy Neutrino Induced Cascades With The Amanda-b10 Detector
title_short Search For High Energy Neutrino Induced Cascades With The Amanda-b10 Detector
title_full Search For High Energy Neutrino Induced Cascades With The Amanda-b10 Detector
title_fullStr Search For High Energy Neutrino Induced Cascades With The Amanda-b10 Detector
title_full_unstemmed Search For High Energy Neutrino Induced Cascades With The Amanda-b10 Detector
title_sort search for high energy neutrino induced cascades with the amanda-b10 detector
publisher Pennsylvania Univ.
publishDate 2002
url http://cds.cern.ch/record/608921
geographic Antarctic
South Pole
The Antarctic
geographic_facet Antarctic
South Pole
The Antarctic
genre Antarc*
Antarctic
Ice cap
South pole
South pole
genre_facet Antarc*
Antarctic
Ice cap
South pole
South pole
op_relation http://cds.cern.ch/record/608921
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