The Voyager data show a decrease in temperature in the inner heliosphere, an increase in temperature from 30–50 AU, a decrease from 50–63 AU, followed by another increase from 63–68 AU. Models of pickup proton heating predict a monotonic temperature rise beyond about 30 AU but do not account for the smaller scale (few AU) temperature variations. At 1 AU, the solar wind temperature is a strong function of the solar wind speed. We find that incorporating a temperature dependence on speed into the pickup proton heating results can reproduce much of the smaller-scale temperature variation observed out to 68 AU. The same speed-temperature dependence provides good fits to data from both the outer heliosphere and from near Earth. Since a large fraction of the proton energy results from heating, this work implies that the heating rate is a function of the speed.
%0 Journal Article
%1 SolarWindTemperatureProfile
%A Richardson, John D.
%A Smith, Charles W.
%D 2003
%I AGU
%J Geophys. Res. Lett.
%K profile solarwind temperature
%N 5
%P 1206--
%R 10.1029/2002GL016551
%T The radial temperature profile of the solar wind
%U http://dx.doi.org/10.1029/2002GL016551
%V 30
%X The Voyager data show a decrease in temperature in the inner heliosphere, an increase in temperature from 30–50 AU, a decrease from 50–63 AU, followed by another increase from 63–68 AU. Models of pickup proton heating predict a monotonic temperature rise beyond about 30 AU but do not account for the smaller scale (few AU) temperature variations. At 1 AU, the solar wind temperature is a strong function of the solar wind speed. We find that incorporating a temperature dependence on speed into the pickup proton heating results can reproduce much of the smaller-scale temperature variation observed out to 68 AU. The same speed-temperature dependence provides good fits to data from both the outer heliosphere and from near Earth. Since a large fraction of the proton energy results from heating, this work implies that the heating rate is a function of the speed.
@article{SolarWindTemperatureProfile,
abstract = {The Voyager data show a decrease in temperature in the inner heliosphere, an increase in temperature from 30–50 AU, a decrease from 50–63 AU, followed by another increase from 63–68 AU. Models of pickup proton heating predict a monotonic temperature rise beyond about 30 AU but do not account for the smaller scale (few AU) temperature variations. At 1 AU, the solar wind temperature is a strong function of the solar wind speed. We find that incorporating a temperature dependence on speed into the pickup proton heating results can reproduce much of the smaller-scale temperature variation observed out to 68 AU. The same speed-temperature dependence provides good fits to data from both the outer heliosphere and from near Earth. Since a large fraction of the proton energy results from heating, this work implies that the heating rate is a function of the speed.},
added-at = {2012-05-07T12:58:16.000+0200},
author = {Richardson, John D. and Smith, Charles W.},
biburl = {https://www.bibsonomy.org/bibtex/29e54db29b7713daa5c2f4b48bec6d3dd/ursg},
description = {The radial temperature profile of the solar wind},
doi = {10.1029/2002GL016551},
interhash = {3139a223e59d2694e1bd6311646ade6c},
intrahash = {9e54db29b7713daa5c2f4b48bec6d3dd},
issn = {00948276},
journal = {Geophys. Res. Lett.},
keywords = {profile solarwind temperature},
month = mar,
number = 5,
pages = {1206--},
publisher = {AGU},
timestamp = {2012-05-07T12:58:16.000+0200},
title = {The radial temperature profile of the solar wind},
url = {http://dx.doi.org/10.1029/2002GL016551},
volume = 30,
year = 2003
}