4.7 Article

The photoheating of the intergalactic medium in synthesis models of the UV background

Journal

MONTHLY NOTICES OF THE ROYAL ASTRONOMICAL SOCIETY
Volume 450, Issue 4, Pages 4081-4097

Publisher

OXFORD UNIV PRESS
DOI: 10.1093/mnras/stv773

Keywords

radiative transfer; methods: numerical; intergalactic medium; quasars: absorption lines; cosmology: theory

Funding

  1. FP7 ERC Advanced Grant Emergence [320596]
  2. Royal Society University Research Fellowship
  3. NSF [OIA-1124453, AST-1229745]
  4. NASA [NNX12A587G]
  5. STFC [ST/I001212/1, ST/K00333X/1, ST/M00418X/1, ST/M007065/1, ST/M006948/1, ST/M007073/1, ST/K000985/1, ST/L000695/1, ST/K000373/1] Funding Source: UKRI
  6. Science and Technology Facilities Council [ST/M00418X/1, ST/K000985/1, ST/M007073/1, ST/M006948/1, ST/L000695/1, ST/M007065/1, ST/K00333X/1, ST/K000373/1] Funding Source: researchfish
  7. Office Of The Director
  8. Office of Integrative Activities [1124453] Funding Source: National Science Foundation

Ask authors/readers for more resources

We compare cosmological hydrodynamical simulations combined with the homogeneous metagalactic UV background (UVB) of Haardt & Madau (hereafter HM2012) to observations of the Lyman alpha forest that are sensitive to the thermal and ionization state of the intergalactic medium (IGM). The transition from optically thick to thin photoheating predicted by the simple one-zone, radiative transfer model implemented by HM2012 predicts a thermal history that is in remarkably good agreement with the observed rise of the IGM temperature at z similar to 3 if we account for the expected evolution of the volume filling factor of He III. Our simulations indicate that there may be, however, some tension between the observed peak in the temperature evolution and the rather slow evolution of the He II opacities suggested by recent Hubble Space Telescope/Cosmic Origins Spectrograph measurements. The HM2012 UVB also underpredicts the metagalactic hydrogen photoionization rate required by our simulations to match the observed opacity of the forest at z > 4 and z < 2.

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