帮我翻译成中文ChinesemeteorologicalsatelliteFY-1Cwassue-cessfullylaunchedon10May1999.TherearetenspectralchannelsinFY-1C,someofwhichsuchaschannel1(0.58-0.68um),channel4(10.3-11.3gym),andchannel6(1.58-1.64},m)ca

Question

帮我翻译成中文
Chinese meteorological satellite FY-1C was sue-
cessfully launched on 10 May 1999. There are ten
spectral channels in FY-1C, some of which such as
channel 1 (0.58-0.68 um), channel 4 (10.3-11.3 gym),
and channel 6 (1.58-1.64 },m) can be used for cloud
particle phase detection. A case study by Liu et al.
(2003x) showed that 1.6 }cm channel could be used to
analyze the thermodynamic phase of cloud particles.
Much more work is needed for the retrieval of cloud
microphysical parameters with Chinese satellite data.
2.4 Video images
The Precipitation Particle Image Sensor (PPIS)
was used to directly observe the cloud microp饰si-
cal structures vertically from the base to the top of
the cloud during the heaviest rainfall of the mei-yu
front in June 1999 (Wang and Yang, 2003). PPIS is a
balloon-borne video-sounder developed by Takahashi
et al. (1995), from which images of precipitation par-
tides larger than 0.5 mm are recorded by a camera. In
addition to the particle images, the PPIS records the
electric charge on the particles and the ambient tem-
perature, humidity, and pressure. The vertical distri-
butions of various cloud particle sizes, number density,
and mass density were retrieved from the observations
by Wang and Yang (2003). Their analyses showed that
ice crystals, graupel, snowflakes and frozen droplets
often coexist with the liquid phase in the convective
cloud clusters in mei-yu front rainband. The inter-
actions of these particles play important roles in the
formation and evohition of rainfall.

Answer 1

中国气象卫星FY-1C是起诉
cessfully发射在1999年5月10日.有十
在FY-1C的鬼渠道,一些
开辟1 (0.58-0.68 um),渠道4 (10.3-11.3体操),
并且渠道6日(1.58-1.64},m)可以为云彩使用
微粒阶段侦查.一个专题研究刘等.
(2003x)表示,1.6} cm渠道可能使用
分析热力学阶段云彩微粒.
更多工作为云彩检索是需要的
与中国卫星数据的microphysical参量.
2.4视频图象
降雨雪微粒图象传感器(PPIS)
使用直接地观察云彩microp饰si-
cal结构垂直从在上面的基地
在mei-yu的最重的降雨量的期间云彩
前面在1999年6月(Wang和杨2003).PPIS是a
takahashi开发的气球出生的录影发声器
等(1995),降雨雪同水准的图象
浪潮大于0.5 mm由照相机记录.在
对微粒图象的加法,PPIS记录
在微粒和四周tem-的电荷
perature、湿气和压力.垂直的distri-
各种各样的云彩微粒大小,数字密度butions,
并且集合密度从观察被检索了
Wang和杨(2003).他们的分析显示了那
冰晶、graupel、雪花和冻结的小滴
经常共存与液体阶段在对流
覆盖在mei-yu前面rainband的群.相互
这些微粒的行动在扮演重要角色
降雨量的形成和evohition.