Search Results
used winds, temperature, and specific humidity from radiosonde data at T3 (3.2°S, 60.6°W). Important supplementary products including apparent heating ( Q 1 ), apparent drying ( Q 2 ), and large-scale vertical motion ( ω ), were obtained from variational analysis ( Tang et al. 2016 ), which are available to the community at the Atmospheric Radiation Measurement (ARM) program archive ( https://iop.archive.arm.gov/arm-iop/0eval-data/xie/scm-forcing/iop_at_mao/GOAMAZON/2014-2015/ ). Twice
used winds, temperature, and specific humidity from radiosonde data at T3 (3.2°S, 60.6°W). Important supplementary products including apparent heating ( Q 1 ), apparent drying ( Q 2 ), and large-scale vertical motion ( ω ), were obtained from variational analysis ( Tang et al. 2016 ), which are available to the community at the Atmospheric Radiation Measurement (ARM) program archive ( https://iop.archive.arm.gov/arm-iop/0eval-data/xie/scm-forcing/iop_at_mao/GOAMAZON/2014-2015/ ). Twice
( Friedl-Vallon et al. 2014 ; Riese et al. 2014 ). For this purpose, GLORIA combines a Michelson interferometer with a 2D infrared detector and measures molecular thermal emissions in the spectral range between 780 and 1,400 cm −1 (7.1–12.8 μ m). GLORIA is mounted in the belly pod. Its line of sight aims toward the horizon on the right side of the aircraft and measures infrared radiation emitted by molecules in the atmosphere. The horizontal observation angle is varied from 45° to 135° with respect
( Friedl-Vallon et al. 2014 ; Riese et al. 2014 ). For this purpose, GLORIA combines a Michelson interferometer with a 2D infrared detector and measures molecular thermal emissions in the spectral range between 780 and 1,400 cm −1 (7.1–12.8 μ m). GLORIA is mounted in the belly pod. Its line of sight aims toward the horizon on the right side of the aircraft and measures infrared radiation emitted by molecules in the atmosphere. The horizontal observation angle is varied from 45° to 135° with respect
.1002/2014JD021460 . Chen , F. , and J. Dudhia , 2001 : Coupling an advanced land surface–hydrology model with the Penn State–NCAR MM5 modeling system. Part I: Model implementation and sensitivity . Mon. Wea. Rev. , 129 , 569 – 585 , doi: 10.1175/1520-0493(2001)129<0569:CAALSH>2.0.CO;2 . Chou , M. , and M. Suarez , 1994 : An efficient thermal infrared radiation parameterization for use in general circulation models. NASA Tech. Memo.104606, 85 pp . Davis , C. , and Coauthors , 2008
.1002/2014JD021460 . Chen , F. , and J. Dudhia , 2001 : Coupling an advanced land surface–hydrology model with the Penn State–NCAR MM5 modeling system. Part I: Model implementation and sensitivity . Mon. Wea. Rev. , 129 , 569 – 585 , doi: 10.1175/1520-0493(2001)129<0569:CAALSH>2.0.CO;2 . Chou , M. , and M. Suarez , 1994 : An efficient thermal infrared radiation parameterization for use in general circulation models. NASA Tech. Memo.104606, 85 pp . Davis , C. , and Coauthors , 2008
