POSSIBLE MICROWAVE-ABSORPTION BY H2S GAS IN URANUS AND NEPTUNE ATMOSPHERES

被引:105
作者
DEPATER, I
ROMANI, PN
ATREYA, SK
机构
[1] SCI SYST & APPLICAT INC,SEABROOK,MD 20706
[2] UNIV MICHIGAN,DEPT ATMOSPHER OCEAN & SPACE SCI,ANN ARBOR,MI 48109
基金
美国国家科学基金会;
关键词
D O I
10.1016/0019-1035(91)90020-T
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
We present new VLA observations of Neptune at 3.55 and 20.1 cm. The disk-averaged brightness temperatures are 191.2 ± 6 K at 3.55 cm, and 276.4 ± 10 K at 20.1 cm. These values are consistent with thermal spectra of the planet. We further present a comparison between Uranus and Neptune's spectrum, using improved atmospheric models for both planets. We improved the old models by including microwave absorption by H2S. The rotational lines of this gas, which are all at (sub)millimeter wavelengths, are pressure broadened to such an extent that considerable opacity at centimeter wavelengths is expected. We estimate from our calculations that the H2S mixing ratio on Uranus and Neptune is likely enhanced by a factor of 10-30 above the solar sulfur elemental ratio, and that the S/N ratio must exceed 5 × the solar ratio. Our calculations suggest the width of the H2S line to be similar to or less than that of water. There is more microwave opacity in Neptune's atmosphere than in that of Uranus, which may be caused by the presence of some NH3 gas above the NH4SH cloud layer. From a comparison with the radio occultation data, we suggest that NH3 is likely supersaturated in Neptune's atmosphere at levels where T ≲ 210-225 K, or P ≲ 20-25 bar. © 1991.
引用
收藏
页码:220 / 233
页数:14
相关论文
共 42 条
[31]   THE ATMOSPHERE OF NEPTUNE - RESULTS OF RADIO OCCULTATION MEASUREMENTS WITH THE VOYAGER-2 SPACECRAFT [J].
LINDAL, GF ;
LYONS, JR ;
SWEETNAM, DN ;
ESHLEMAN, VR ;
HINSON, DP ;
TYLER, GL .
GEOPHYSICAL RESEARCH LETTERS, 1990, 17 (10) :1733-1736
[32]   THE ATMOSPHERE OF URANUS - RESULTS OF RADIO OCCULTATION MEASUREMENTS WITH VOYAGER-2 [J].
LINDAL, GF ;
LYONS, JR ;
SWEETNAM, DN ;
ESHLEMAN, VR ;
HINSON, DP ;
TYLER, GL .
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 1987, 92 (A13) :14987-15001
[33]   THE SPECTRA OF URANUS AND NEPTUNE AT 8-14 AND 17-23 MU-M [J].
ORTON, GS ;
AITKEN, DK ;
SMITH, C ;
ROCHE, PF ;
CALDWELL, J ;
SNYDER, R .
ICARUS, 1987, 70 (01) :1-12
[34]   THE ALBEDO, EFFECTIVE TEMPERATURE, AND ENERGY-BALANCE OF URANUS, AS DETERMINED FROM VOYAGER IRIS DATA [J].
PEARL, JC ;
CONRATH, BJ ;
HANEL, RA ;
PIRRAGLIA, JA ;
COUSTENIS, A .
ICARUS, 1990, 84 (01) :12-28
[35]  
POLLACK JB, 1989, ORIGIN EVOLUTION PLA, P564
[36]  
POYNTER RL, 1981, JPL PUBLICATION, V8023
[37]  
Pruppacher H. R., 1999, J ATMOS CHEM, V32, P420, DOI DOI 10.1023/A:1000652616430
[38]   NEPTUNE DEEP ATMOSPHERE REVEALED [J].
ROMANI, PN ;
DEPATER, I ;
ATREYA, SK .
GEOPHYSICAL RESEARCH LETTERS, 1989, 16 (08) :933-936
[39]  
SRAMEK RA, 1989, SYNTHESIS IMAGING RA, P117
[40]   ENERGETIC CHARGED-PARTICLES IN THE MAGNETOSPHERE OF NEPTUNE [J].
STONE, EC ;
CUMMINGS, AC ;
LOOPER, MD ;
SELESNICK, RS ;
LAL, N ;
MCDONALD, FB ;
TRAINOR, JH ;
CHENETTE, DL .
SCIENCE, 1989, 246 (4936) :1489-1494