sheeny
27-07-2006, 07:08 AM
I got this from this morning's Nature Contents.
Enjoy,
Al.
Editor's Summary
27 July 2006
It's raining methane
Saturn's moon Titan and the Earth are the only Solar System worlds where rain reaches the surface. Titan's rain may not be much like ours, as it's methane rain, and the atmospheric cycles of water and methane are very different. Two papers this week offer clues as to what a rainy day on Titan might be like. Hueso and Sánchez-Lavega use a numerical model to show that severe methane convective storms accompanied by intense precipitation may occur in certain conditions. These storms would be comparable to flash flood events on Earth. Tokano et al. present methane distribution and temperature data from instruments on board the Huygens probe. Huygens recently took images of landscapes suggestive of rivers or lake-beds, but the camera did not show any liquid. The new data point to the presence of weak drizzle-like rain. In contrast to clouds observed by telescopes or the Cassini spacecraft, the barely visible clouds encountered by Huygens are widespread, suggesting that rainfall occurs globally and may affect Titan's surface structures.
News and Views: Planetary science: Titan's exotic weather
Titan is viewed as a sibling of Earth, as both bodies have rainy weather systems and landscapes formed by rivers. But as we study these similarities, Titan emerges as an intriguingly foreign world.
Caitlin A. Griffith
Letter
Nature 442, 428-431(27 July 2006) | doi:10.1038/nature04933; Received 6 February 2006; Accepted 23 May 2006
Methane storms on Saturn's moon Titan
R. Hueso1 (http://www.nature.com/nature/journal/v442/n7101/abs/nature04933.html#a1) and A. Sánchez-Lavega1 (http://www.nature.com/nature/journal/v442/n7101/abs/nature04933.html#a1)
Top of page (http://www.nature.com/nature/journal/v442/n7101/abs/nature04933.html#top) The presence of dry fluvial river channels and the intense cloud activity in the south pole of Titan over the past few years1,2,3 suggest the presence of methane rain. The nitrogen atmosphere of Titan therefore appears to support a methane meteorological cycle that sculptures the surface and controls its properties1,4. Titan and Earth are the only worlds in the Solar System where rain reaches the surface, although the atmospheric cycles of water and methane are expected to be very different5. Here we report three-dimensional dynamical calculations showing that severe methane convective storms accompanied by intense precipitation may occur in Titan under the right environmental conditions. The strongest storms grow when the methane relative humidity in the middle troposphere is above 80 per cent, producing updrafts with maximum velocities of 20 m s-1, able to reach altitudes of 30 km before dissipating in 5–8 h. Raindrops of 1–5 mm in radius produce precipitation rainfalls on the surface as high as 110 kg m-2 and are comparable to flash flood events on Earth6.
Letter
Nature 442, 432-435(27 July 2006) | doi:10.1038/nature04948; Received 29 March 2006; Accepted 6 June 2006
Methane drizzle on Titan
Tetsuya Tokano1 (http://www.nature.com/nature/journal/v442/n7101/abs/nature04948.html#a1), Christopher P. McKay2 (http://www.nature.com/nature/journal/v442/n7101/abs/nature04948.html#a2), Fritz M. Neubauer1 (http://www.nature.com/nature/journal/v442/n7101/abs/nature04948.html#a1), Sushil K. Atreya3 (http://www.nature.com/nature/journal/v442/n7101/abs/nature04948.html#a3), Francesca Ferri4 (http://www.nature.com/nature/journal/v442/n7101/abs/nature04948.html#a4), Marcello Fulchignoni5 (http://www.nature.com/nature/journal/v442/n7101/abs/nature04948.html#a5),6 (http://www.nature.com/nature/journal/v442/n7101/abs/nature04948.html#a6) and Hasso B. Niemann7 (http://www.nature.com/nature/journal/v442/n7101/abs/nature04948.html#a7)
Top of page (http://www.nature.com/nature/journal/v442/n7101/abs/nature04948.html#top) Saturn's moon Titan shows landscapes with fluvial features1 suggestive of hydrology based on liquid methane. Recent efforts in understanding Titan's methane hydrological cycle have focused on occasional cloud outbursts near the south pole2,3,4 or cloud streaks at southern mid-latitudes5,6 and the mechanisms of their formation. It is not known, however, if the clouds produce rain or if there are also non-convective clouds, as predicted by several models7,8,9,10,11. Here we show that the in situ data on the methane concentration and temperature profile in Titan's troposphere point to the presence of layered optically thin stratiform clouds. The data indicate an upper methane ice cloud and a lower, barely visible, liquid methane-nitrogen cloud, with a gap in between. The lower, liquid, cloud produces drizzle that reaches the surface. These non-convective methane clouds are quasi-permanent features supported by the global atmospheric circulation, indicating that methane precipitation occurs wherever there is slow upward motion. This drizzle is a persistent component of Titan's methane hydrological cycle and, by wetting the surface on a global scale, plays an active role in the surface geology of Titan.
Enjoy,
Al.
Editor's Summary
27 July 2006
It's raining methane
Saturn's moon Titan and the Earth are the only Solar System worlds where rain reaches the surface. Titan's rain may not be much like ours, as it's methane rain, and the atmospheric cycles of water and methane are very different. Two papers this week offer clues as to what a rainy day on Titan might be like. Hueso and Sánchez-Lavega use a numerical model to show that severe methane convective storms accompanied by intense precipitation may occur in certain conditions. These storms would be comparable to flash flood events on Earth. Tokano et al. present methane distribution and temperature data from instruments on board the Huygens probe. Huygens recently took images of landscapes suggestive of rivers or lake-beds, but the camera did not show any liquid. The new data point to the presence of weak drizzle-like rain. In contrast to clouds observed by telescopes or the Cassini spacecraft, the barely visible clouds encountered by Huygens are widespread, suggesting that rainfall occurs globally and may affect Titan's surface structures.
News and Views: Planetary science: Titan's exotic weather
Titan is viewed as a sibling of Earth, as both bodies have rainy weather systems and landscapes formed by rivers. But as we study these similarities, Titan emerges as an intriguingly foreign world.
Caitlin A. Griffith
Letter
Nature 442, 428-431(27 July 2006) | doi:10.1038/nature04933; Received 6 February 2006; Accepted 23 May 2006
Methane storms on Saturn's moon Titan
R. Hueso1 (http://www.nature.com/nature/journal/v442/n7101/abs/nature04933.html#a1) and A. Sánchez-Lavega1 (http://www.nature.com/nature/journal/v442/n7101/abs/nature04933.html#a1)
Top of page (http://www.nature.com/nature/journal/v442/n7101/abs/nature04933.html#top) The presence of dry fluvial river channels and the intense cloud activity in the south pole of Titan over the past few years1,2,3 suggest the presence of methane rain. The nitrogen atmosphere of Titan therefore appears to support a methane meteorological cycle that sculptures the surface and controls its properties1,4. Titan and Earth are the only worlds in the Solar System where rain reaches the surface, although the atmospheric cycles of water and methane are expected to be very different5. Here we report three-dimensional dynamical calculations showing that severe methane convective storms accompanied by intense precipitation may occur in Titan under the right environmental conditions. The strongest storms grow when the methane relative humidity in the middle troposphere is above 80 per cent, producing updrafts with maximum velocities of 20 m s-1, able to reach altitudes of 30 km before dissipating in 5–8 h. Raindrops of 1–5 mm in radius produce precipitation rainfalls on the surface as high as 110 kg m-2 and are comparable to flash flood events on Earth6.
Letter
Nature 442, 432-435(27 July 2006) | doi:10.1038/nature04948; Received 29 March 2006; Accepted 6 June 2006
Methane drizzle on Titan
Tetsuya Tokano1 (http://www.nature.com/nature/journal/v442/n7101/abs/nature04948.html#a1), Christopher P. McKay2 (http://www.nature.com/nature/journal/v442/n7101/abs/nature04948.html#a2), Fritz M. Neubauer1 (http://www.nature.com/nature/journal/v442/n7101/abs/nature04948.html#a1), Sushil K. Atreya3 (http://www.nature.com/nature/journal/v442/n7101/abs/nature04948.html#a3), Francesca Ferri4 (http://www.nature.com/nature/journal/v442/n7101/abs/nature04948.html#a4), Marcello Fulchignoni5 (http://www.nature.com/nature/journal/v442/n7101/abs/nature04948.html#a5),6 (http://www.nature.com/nature/journal/v442/n7101/abs/nature04948.html#a6) and Hasso B. Niemann7 (http://www.nature.com/nature/journal/v442/n7101/abs/nature04948.html#a7)
Top of page (http://www.nature.com/nature/journal/v442/n7101/abs/nature04948.html#top) Saturn's moon Titan shows landscapes with fluvial features1 suggestive of hydrology based on liquid methane. Recent efforts in understanding Titan's methane hydrological cycle have focused on occasional cloud outbursts near the south pole2,3,4 or cloud streaks at southern mid-latitudes5,6 and the mechanisms of their formation. It is not known, however, if the clouds produce rain or if there are also non-convective clouds, as predicted by several models7,8,9,10,11. Here we show that the in situ data on the methane concentration and temperature profile in Titan's troposphere point to the presence of layered optically thin stratiform clouds. The data indicate an upper methane ice cloud and a lower, barely visible, liquid methane-nitrogen cloud, with a gap in between. The lower, liquid, cloud produces drizzle that reaches the surface. These non-convective methane clouds are quasi-permanent features supported by the global atmospheric circulation, indicating that methane precipitation occurs wherever there is slow upward motion. This drizzle is a persistent component of Titan's methane hydrological cycle and, by wetting the surface on a global scale, plays an active role in the surface geology of Titan.