Bibcode
Sicard, Michaël; Md Reba, M. Nadzri; Tomás, Sergio; Comerón, Adolfo; Batet, Oscar; Muñoz-Porcar, Constantino; Rodríguez, Alejandro; Rocadenbosch, Francisco; Muñoz-Tuñón, C.; Fuensalida, J. J.
Bibliographical reference
Monthly Notices of the Royal Astronomical Society, Volume 405, Issue 1, pp. 129-142.
Advertised on:
6
2010
Citations
4
Refereed citations
3
Description
Because of the high quality of its sky, the Roque de los Muchachos
Observatory (ORM), located on the island of La Palma in the Canary
Islands, is home to many astronomical facilities. In the context of the
Extremely Large Telescope Design Study, two intensive lidar campaigns
were performed at the ORM near the Jacobus Kapteyn Telescope between
2007 July 9 and 11 and between 2008 May 26 and June 14. The goal of the
campaign was to characterize the atmosphere in terms of the height of
the planetary boundary layer (PBL) and the aerosol stratification versus
synoptic conditions. Three typical synoptic situations were found, which
supported the intrusion of aerosols from marine/oceanic, anthropogenic
and Saharan origins, respectively. All measurements revealed a
multilayer stratification with a mean PBL height of 546 +/- 198 m agl
and top layers as high as ~8400 m asl. As a by-product, an estimate of
the aerosol optical thickness was also obtained and compared to the
total atmospheric extinction coefficient measured by the Carlsberg
Meridian Telescope. Except in the presence of Saharan dust, the aerosol
optical thickness is very low; the average values are 0.0405 at 532 nm
and 0.0055 at 1064 nm. In the presence of Saharan dust, values of 0.233
and 0.157 were found at 532 and 1064 nm, respectively. The proportion of
aerosol optical thickness contained in the layers above the PBL against
that contained in the PBL is in all cases greater or equal to 50 per
cent. This emphasizes the importance of the upper layers in the
scattering and absorption of astronomical signals. Additionally, for the
first time, spaceborne lidar measurements were also compared to those of
a ground lidar, in order to evaluate the use of a spaceborne active
instrument for aerosol content monitoring at an astronomical site.