Vertical mass and moisture structure from TIROS-N

During the First Global GARP Experiment (FGGE), global determinations of mass and moisture were made from TIROS-N (and NOAA-6) infrared and microwave sounding radiance measurements. At NESS in Washington, the meteorological data were produced operationally with a horizontal resolution of 250 km for inclusion in the FGGE level II-b data sets intended for application to large scale numerical analysis and prediction models. High horizontal resolution (50 km) sounding data sets are being produced by NESS and the Space Science and Engineering Center at the University of Wisconsin and at the NASA/Goddard Space Flight Center for special case studies of the “Special Observing Periods” of FGGE.Results are presented to display the characteristics of the sounding data at different resolutions. For the low horizontal resolution data, an evaluation is shown by comparisons of global analyses made only from satellite soundings over land and sea, and those made operationally by the National Meteorological Center, which excluded satellite sounding data over continental areas, but included all conventional data sources. For the high horizontal resolution sounding data, results are presented to demonstrate the delineation of small scale temperature and moisture features which are consistent with the meteorological processes involved.     

Numerical simulation—assessment of FGGE data with regard to their assimilation in a global data set

The data-assimilation system at the European Centre for Medium Range Forecasts (ECMWF) is presented. The data assimilation system is used to process the FGGE level II-b data and to provide global 3-dimensional analyses for every 6th hour through the whole FGGE year. The quality and the excellent coverage of the data has meant a substantial improvement in our understanding of the global atmosphere with major implication for climate and extended weather forecasting.Results from an observing system experiment only using data observed and collected from space is presented. It is found that fully space-oriented systems are possible although forecast quality is higher in areas where radiosondes are available with a satisfactory density.     

The role of space techniques in FGGE

The space-based sub-system of the composite observing system, operated during the Operational Year of the Global Weather Experiment, played an indispensable role in the acquisition of data and in transmitting data from surface-based and airborne observational platforms to data-processing centres. The sub-system comprised both geostationary and near-polar orbiting meteorological satellites and special efforts were undertaken to keep the performance of the system as close as possible to that which had been anticipated during the planning stage of the Experiment.Five geostationary satellites were spaced at approximately uniform intervals around the equator. They were used primarily to derive wind vectors by measuring the displacement of clouds. The satellites also provided communication support for the Aircraft to Satellite Data Relay system, by which flight level meteorological data were automatically transmitted to ground receiving stations.Three polar orbiting satellites provided data simultaneously during the whole Operational Year. Vertical temperature soundings, clear-radiance data, sea-surface temperature and wind speed data, and total atmospheric water vapour data were produced for inclusion in the research data set of the Experiment. Two of these satellites /TIROS-N and NOAA-6/ carried a new data collection and platform location system, a basic component of the Tropical Constant Level Balloon System and the Drifting Buoy System of FGGE.     

The limb infrared monitor of the stratosphere (LIMS) experiment: Temperature and nitrogen dioxide results

The Limb Infrared Monitor of the Stratosphere (LIMS) is a 6 channel scanning radiometer which measures the infrared emission by the earth's limb. These measurements are inverted to yield distributions of temperature, ozone, water vapor, nitric acid and nitrogen dioxide. The instrumentation and its orbital performance are briefly described. Retrievals of temperature and nitrogen dioxide are presented, with a discussion of their precision. Comparisons to in-situ rocket and balloon measurements are used to assess their accuracy. Special mention is made of the temperature data supplied for the FGGE II-b data sets. Results for ozone, water vapor and nitric acid are presented in companion papers.     

Satellite-derived synoptic climatology in data-sparse regions

Synoptic-scale “moisture bursts” are defined, based on infrared GOES imagery, and their synoptic climatology is developed. Quantitative analysis of satellite-derived individual channel radiance data and vertical eigenfunctions of complete channel data yield rich structural detail; these details do not appear in FGGE analyses in regions void of conventional meteorological data.     

Impact of FGGE buoy system data on southern hemisphere meteorology

Although a definitive evaluation of the performance of the FGGE buoy system will take some time, it is already clear that the buoy data have made a major contribution to both operational and research aspects of southern hemisphere meteorology. The buoys have provided a wealth of information on both the surface drift and sea surface temperature characteristics of the Southern Ocean. Their impact on operational synoptic analysis and prediction in the southern hemisphere during the FGGE year was substantial. The buoy pressure data generally provided an adequate basis for delineation of the large scale flow over the middle and high latitude oceans in a way that has not been possible before. Preliminary evaluations of the impact of the buoy data on numerical prediction have indicated small but significant improvements in skill scores. Regional Forecasting Centres in the southern States of Australia have found that the more accurate delineation of synoptic systems over the oceans to the south has contributed significantly to forecast performance in their Regions. Use of the buoy data, and synoptic analyses based on the buoy data, to examine particular problems in southern hemisphere meteorology is now underway.     

Geostationary operational environmental satellite system performance

The United States supported the First GARP Global Experiment (FGGE) by the use of three geostationary satellites: GOES-East, located at 75°W longitude, GOES-West at 135°W longitude, and, through a special cooperative effort by the National Oceanic and Atmospheric Administration, the National Aeronautics and Space Administration, and the European Space Agency, GOES-Indian Ocean at 58°E longitude. During the FGGE Operational Year, the GOES-East coverage was provided, in turn, by GOES-2, SMS-1, and SMS-2. The GOES-West coverage was provided by GOES-3, and GOES-1 served at the GOES-Indian Ocean location. Satellite and instrument performance was generally satisfactory during that period except for the loss of infrared data from the Indian Ocean GOES for an aggregate of 31 days due to intermittent operation of the sensor. From the GOES-East and GOES-West data, the National Environmental Satellite Service produced cloud motion vectors for 0000, 1200, and 1800 GMT daily, numbering in total about 1400 vectors per day. High resolution wind vectors at the rate of somewhat under 3000 daily were derived from the data from all three satellites in the tropical zone bounded by 15°N and 15°S latitude by the University of Wisconsin. In addition to their contributions to the FGGE research data sets, these three satellites provided other real-time benefits and services.     

Measurements of the earth radiation budget from satellites during the first garp global experiment

Two special measurements of the energy exchange between earth and space were made in connection with the FGGE. A global monitoring program using wide-field-of-view and scanner detectors from NASA's NIMBUS-7 satellite successfully returned measurements during the entire FGGE. This experiment system also used a black cavity detector to measure the total energy output of the sun to very high precision. A second set of high frequency time and space estimates of the radiation budget were determined from selected geostationary satellite data. Preliminary results from both radiation budget data sets and the solar “constant” measurements will be presented.     

WMO FGGE navaid system

To meet the scientific objectives of the Global Weather Experiment (FGGE) the availability of the detailed vertical wind structure especially in the tropics was considered to be crucial. The Tropical Wind Observing Ships (TWOS) System was implemented to supplement the land-based data during FGGE. Many of the ships which participated in this observing system did not have upper-air observing equipment on board. A Navaid-based sounding system was developed and purchased for these ships through WMO co-ordination and international funding.The paper describes the principles of the Navaid windfinding technique, the hardware solution for the WMO FGGE Navaid Sounding System, the implementation of Navaid data collection and processing, and an assessment of the quality of data acquired.     

Seasonal-to-interannual variability of chlorophyll-a bloom timing associated with physical forcing in the Gulf of Cádiz

Seasonal-to-interannual variability of the winter-spring bloom in the Gulf of Cádiz, eastern North Atlantic, has been investigated using chlorophyll-a remote sensing (CHL). These data have been obtained from the GlobColour project; the temporal coverage extends from September 1997 to December 2010. In this study we develop a generic quantitative approach for describing the temporal variability in the shape of the winter-spring bloom within a region. Variability in both the timing and magnitude of the bloom in the basin has been evaluated as a function of physical properties in the water column such as Mixed Layer Depth (MLD, GODAS model), sea surface temperature (SST, from AVHRR radiometers), photosynthetically-active radiation (PAR, from ocean color data) and euphotic depth (Z_eu, from ocean color data). The analysis indicated that the timing, size and duration of the phytoplankton bloom in this area are largely controlled by both meteorological and oceanographic conditions at different scales; this means that it is likely to vary widely from one year to another.     

The FGGE—Scientific objectives and preliminary assessment of operations

The scientific objectives of the FGGE and the observational requirements prescribed for the experiment are reviewed. The performance of the observational systems implemented for the operational year is summarised for each component and the extent to which the composite observing system met the requirements is assessed. It is concluded that although the formal requirements were not strictly reached over the whole globe, nevertheless exceptional enhancement was achieved in the areas normally observed very inadequately and it is judged that the final data sets will allow the scientific objectives of the FGGE to be attained. This conclusion depends crucially on the satellite contributions, especially those of TIROS-N.     

The compatability of cloud tracked winds from the United States,European, and Japanese geostationary satellites

Overlap of coverage of the five geostationary satellites has allowed an intercomparison of the FGGE cloud tracked winds. No attempt was made during FGGE to standardize the cloud tracking techniques. In spite of this potential for differences between data sets, the compatability of the various cloud wind data sets was generally quite good. The vector magnitude differences between nearly co-located vectors showed similar cumulative frequency statistics for all data producers. A study of systematic biases which could affect a global wind analysis of any given synoptic period showed that image alignment errors caused less than 2 m s^?1 bias for all data producers except the NESS high level winds which had an average bias of slightly greater than 3 m s^?1. This appears to be caused by the manual alignment of images in the movie loops. Height bias studies showed the Japanese winds to be higher than other data producers by as much as 100 mb for both the high and low levels winds. Height biases appear to be caused by the differences in cloud wind height assignment procedures.     

Athens Neutron Monitor Data Processing Center – ANMODAP Center

Cosmic ray measurements in Athens were initiated in November 2000 with a standard 6NM-64 neutron monitor. Within the last years an effort has been made in order to construct an effective database of neutron monitor (NM) and satellite data in real-time, regarding the necessities of space weather monitoring (Athens Neutron Monitor Data Processing Center – ANMODAP Center). The prospective goal of this network is to make possible the receiving of all data in real-time in close sequence from all servers around the globe. The graphical representation of all these data in real-time is available through the website of the station (http://cosray.phys.uoa.gr). Moreover, a second database that collects data with 1-min resolution operates in a parallel mode. The online services as a special ‘Alert’ algorithm for Ground Level Enhancements (GLEs) and some models created to analyze aspects of GLEs as the neutron monitor Basic Anisotropic Neutron Ground Level Enhancement (BANGLE) model and the Forbush Decreases (FORD) model as well, are presented. Moreover, a short account on work performed on the possible relationship between the geomagnetic activity level and the biological effects is given.     

Real-time stereoscopic applications using the goes operational satellites

We have investigated the use of real and synthetic stereo satellite images and stereo graphics in applications such as cloud-tracked winds, severe storm cloud analysis, and general meteorological interpretation. We have concluded that a stereo meteorological presentation is possible and desirable in an operational environment. Synthetic stereo could be used immediately in cloud-tracked wind operations. The presentation allows one to appreciate the interrelations between cloud motions and cloud structures, especially in multi-layered situations. Reprocessing of FGGE tropical wind sets with a synthetic stereo presentation showed some improved yields of low-level vectors, a significant increase in mid-level vectors, and very little change in the high-level vectors. Severe local storm real-stereo presentations are possible operationally because the 15 minute RISOP operations of GOES-East allow simultaneous scanning of both geosynchronous satellites twice per hour. The real-stereo height measurements of overshooting turrets are an improvement over infrared heights and can be used to monitor the strength of the thunderstorm updraft. Synthetic stereo presentations of thunderstorm tops can be presented in a non-linear fashion which stretches out the cloud top features. The synthetic stereo presentation is easier for most people to see. We recommend the use of a hybrid system where the viewing is done on the synthetic stereo image and the quantitative measurements are done on the real-stereo pairs.     

静止气象卫星的功能及姿态稳定方式对功能的影响

<正> 一、前言国际电信联盟无线电规则把气象卫星业务定义为用于气象目的的地球探测卫星业务。但对静止气象卫星业务来说,气象业务部门希望它不仅要具有气象观测功能,而且要具有收集、传送和分发各种气象信息的功能。因此,静止气象卫星不仅是位于静止轨道上的空间气象观测平台,而且也是收集,传送和分发气象数据的中继站,其有效载荷主要是观测地球大气的各种遥感仪器及收集、传送和分发气象数据的通信系统。它兼有地球探测卫星和通信卫星的     

Ocean circulation studies in the vicinity of Southern Africa: Preliminary results using FGGE drifters and remote sensing

The three highly variable ocean circulation systems which meet south of South Africa have been studied by combining the use of satellite thermal infra-red imagery, hydrographic measurements and drifting buoys. We present a few preliminary examples where this method has been successful. These include the sources of the Agulhas Current, the influence of the Agulhas Current on the Cape upwelling region as well as the interaction of the Agulhas Current with the Subtropical Convergence. An example is also given of how a biological hypothesis concerning the recruitment of a rock lobster species at Vema Seamount has been supported by the analysis of the drifts of FGGE buoys in the South Atlantic Ocean.     

First quality assessment of the Cryosat-2 altimetric system over ocean

This paper presents the results of a Calval analysis performed for the Cryosat-2 mission over ocean. The data set used in this analysis consists of products generated by the Cryosat-2 Processor Prototype developed by CNES (Center National d’Etudes Spatiales). This data set has been analysed focusing on LRM (Low Resolution Mode) mode only. One major objective of this paper is to illustrate the potential of Cryosat-2 data over ocean, mainly for waves and Sea Level Anomaly applications. All the results indicate very good performances of the SIRAL (SAR/Interferometric Altimeter) altimeter over ocean. Crossover standard deviation is close to 6.5 cm over the analysed period (3 months) which is close to the Jason-2 and ENVISAT performance. All these results confirm that Cryosat’s altimeter can provide data almost as valuable as other flying altimetric missions, and that it has the potential to contribute to oceanography (e.g. multi-mission climate record, mesoscale monitoring in near real time) and to geodesy (e.g. mean sea surface, bathymetry).     

A study of the onset of the Indian monsoon as seen from GEOS I.O. satellite

Wind fields deduced from cloud motions are extracted by an optical method from GOES I.O. pictures during FGGE : 1–10 February 1979, 16 May – 7 July 1979. These winds are compared with in-situ measurements with dropsondes. The onset of the monsoon is described from the point of view of winds and cloud cover.     

CRESDA APPLICATION SYSTEM OF CBERS-1, RESULTS AND TYPICAL EXAMPLES OF APPLICATIONS

CRESDA Application System of CBERS-1 was established in 1999. During the operation of the system for more than two years, about 240 000 scenes of CBERS-1 Level 0 data have been archived and more than 13 000 scenes of Level 2 products have been ordered by end users from different application fields.In this paper, the typical examples of applications in crop yield estimation,calamity alleviation, resources survey and protection, environment monitoring and continuable development, and urban planning are mainly described.