Cloud water contents and hydrometeor sizes during the FIRE Arctic Clouds Experiment

被引:61
作者
Shupe, MD
Uttal, T
Matrosov, SY
Frisch, AS
机构
[1] NOAA, Environm Technol Lab, Sci & Technol Corp, Boulder, CO USA
[2] Univ Colorado, NOAA, Environm Technol Lab, Cooperat Inst Res Environm Sci, Boulder, CO USA
[3] Colorado State Univ, NOAA, Environm Technol Lab, Cooperat Inst Res Atmosphere, Boulder, CO USA
关键词
D O I
10.1029/2000JD900476
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
During the year-long Surface Heat Budget of the Arctic Experiment (1997-1998) the NOAA Environmental Technology Laboratory operated a 35-GHz cloud radar and the DOE Atmospheric Radiation Measurement Program operated a suite of radiometers at an ice station frozen into the drifting ice pack of the Arctic Ocean. The NASA/FIRE Arctic Clouds Experiment took place during April-July 1998, with the primary goal of investigating cloud microphysical, geometrical, and radiative properties with aircraft and surface-based measurements. In this paper, retrieval techniques are utilized which combine the radar and radiometer measurements to compute height-dependent water contents and hydrometeor sizes for all-ice and all-liquid clouds. For the spring and early summer period, all-ice cloud retrievals showed a mean particle diameter of about 60 mum and ice water contents up to 0.1 g/m(3), with the maximum sizes and water contents at approximately one fifth of the cloud depth from the cloud base. The all-liquid cloud retrievals had a mean effective particle radius of 7.4 mum, liquid water contents up to 0.7 g/m(3), and a mean droplet concentration of 54 cm(-3). Maximum retrieved liquid drop sizes, water contents, and concentrations occurred at three fifths of the cloud depth from the cloud base. As a measure of how representative the FIRE-ACE aircraft flight days were of the April-July months in general, retrieval statistics for flight-day clouds are compared to the mean retrieval statistics. From the retrieval perspective the ice particle sizes and water contents on flight days were similar to 30% larger than the mean retrieved values for the April-July months. Retrieved liquid cloud parameters during flight days were all about 20% smaller. All-ice and/or all-liquid clouds acceptable for these retrieval techniques were observed about 34% of the time clouds were present; at all other times, mixed-phase clouds precluded the use of these single-phase retrieval techniques.
引用
收藏
页码:15015 / 15028
页数:14
相关论文
共 42 条
[21]  
2
[22]  
Matrosov SY, 1998, J ATMOS OCEAN TECH, V15, P184, DOI 10.1175/1520-0426(1998)015<0184:COICPO>2.0.CO
[23]  
2
[24]   Variability of microphysical parameters in high-altitude ice clouds: Results of the remote sensing method [J].
Matrosov, SY .
JOURNAL OF APPLIED METEOROLOGY, 1997, 36 (06) :633-648
[25]   Retrievals of vertical profiles of ice cloud microphysics from radar and IR measurements using tuned regressions between reflectivity and cloud parameters [J].
Matrosov, SY .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1999, 104 (D14) :16741-16753
[26]  
MATROSOV SY, 1994, J APPL METEOROL, V33, P617, DOI 10.1175/1520-0450(1994)033<0617:ROVPOC>2.0.CO
[27]  
2
[28]   ESTIMATION OF ICE-CLOUD PARAMETERS FROM GROUND-BASED INFRARED RADIOMETER AND RADAR MEASUREMENTS [J].
MATROSOV, SY ;
UTTAL, T ;
SNIDER, JB ;
KROPFLI, RA .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1992, 97 (D11) :11567-11574
[29]  
Moran KP, 1998, B AM METEOROL SOC, V79, P443, DOI 10.1175/1520-0477(1998)079<0443:AUCPRF>2.0.CO
[30]  
2