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2018

4927 record(s)
 
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  • ---- The bulletin is coded as BUFR code form: FM 94 (BUFR, Binary universal form for the representation of meteorological data) . (Refer to WMO No.306 - Manual on Codes for the definition of WMO international codes) ---- The IUCN07TTAAii Data Designators decode (2) as: T1 (I): Observational data (Binary coded) - BUFR. T2 (U): Upper air. A1 (C): (used for single level satellite-derived reports - see Note 3) A2 (N): Northern hemisphere. (2: Refer to WMO No.386 - Manual on the GTS - Attachment II.5) ---- Correspondence with the C13 common BUFR/CREX code table: (005/000) or (Single level upper-air data (satellite) -- AMV) data type / data sub-type. ---- WMO No.9 - Volume C1 'Remarks' field: Atmospheric Motion Vectors (Infrared Channel 1) (NORTHERN HEMISPHERE); NOTE: FROM COMS (128.2° E)

  • ---- The bulletin is coded as BUFR code form: FM 94 (BUFR, Binary universal form for the representation of meteorological data) . (Refer to WMO No.306 - Manual on Codes for the definition of WMO international codes) ---- The IUCN10 TTAAii Data Designators decode (2) as: T1 (I): Observational data (Binary coded) - BUFR. T2 (U): Upper air. A1 (C): (used for single level satellite-derived reports - see Note 3) A2 (N): Northern hemisphere. (2: Refer to WMO No.386 - Manual on the GTS - Attachment II.5) ---- Correspondence with the C13 common BUFR/CREX code table: (005/000) or (Single level upper-air data (satellite) -- AMV) data type / data sub-type. ---- WMO No.9 - Volume C1 'Remarks' field: Atmospheric Motion Vectors (Infrared Channel 1) (NORTHERN HEMISPHERE); NOTE: FROM COMS (128.2° E)

  • ---- The IUKC03 TTAAii Data Designators decode (2) as: T1 (I): Observational data (Binary coded) - BUFR. T2 (U): Upper air. A1 (K): Radio soundings from fixed land stations (up to 100 hPa) TEMP (parts A, B). A2 (C): 180° - 90°E northern hemisphere. (2: Refer to WMO No.386 - Manual on the GTS - Attachment II.5) ---- Correspondence with the C13 common BUFR/CREX code table: (002/004) or (Vertical soundings (other than satellite) -- Upper-level temperature/humidity/wind reports from fixed-land stations (TEMP)) data type / data sub-type. ---- The bulletin collects reports from stations: 47104(BUKGANGNEUNG ) ---- This bulletin is related with bulletin IUSC03RKSL

  • ---- The IUKC05 TTAAii Data Designators decode (2) as: T1 (I): Observational data (Binary coded) - BUFR. T2 (U): Upper air. A1 (K): Radio soundings from fixed land stations (up to 100 hPa) TEMP (parts A, B). A2 (C): 180° - 90°E northern hemisphere. (2: Refer to WMO No.386 - Manual on the GTS - Attachment II.5) ---- Correspondence with the C13 common BUFR/CREX code table: (002/004) or (Vertical soundings (other than satellite) -- Upper-level temperature/humidity/wind reports from fixed-land stations (TEMP)) data type / data sub-type. ---- The bulletin collects reports from stations: 47169 (HEUKSANDO) --- This bulletin is related with bulletin IUSC05RKSL

  • ---- The bulletin is coded as BUFR code form: FM 94 (BUFR, Binary universal form for the representation of meteorological data) . (Refer to WMO No.306 - Manual on Codes for the definition of WMO international codes) ---- The IUCN38 TTAAii Data Designators decode (2) as: T1 (I): Observational data (Binary coded) - BUFR. T2 (U): Upper air. A1 (C): (used for single level satellite-derived reports - see Note 3) A2 (N): Northern hemisphere. (2: Refer to WMO No.386 - Manual on the GTS - Attachment II.5) ---- Correspondence with the C13 common BUFR/CREX code table: (005/000) or (Single level upper-air data (satellite) -- AMV) data type / data sub-type. ---- WMO No.9 - Volume C1 'Remarks' field: Atmospheric Motion Vectors (Infrared Channel 1) (NORTHERN HEMISPHERE); NOTE: FROM COMS (128.2° E)

  • ---- The bulletin collects SHIP reports: FM 13 (SHIP, Report of surface observation from a sea station). (Refer to WMO No.306 - Manual on Codes for the definition of WMO international codes) ---- The SMVX02 TTAAii Data Designators decode (2) as: T1 (S): Surface data. T2 (M): Main synoptic hour. A1 (V): Mobile ships and other marine stations. A2 (X): More than one area. (2: Refer to WMO No.386 - Manual on the GTS - Attachment II.5) ---- The bulletin collects reports from stations: ship

  • NARVAL-South: Measurements of microwave radiometer brightness temperatures, radar reflectivity and linear depolarisation ratio, and dropsonde atmospheric profiles from aircraft campaign over tropical Atlantic out of Barbados. Aim of the campaign was the observation of shallow convection in the trade wind region east of Barbados. website: http://www.mpimet.mpg.de/en/science/the-atmosphere-in-the-earth-system/working-groups/tropical-cloud-observation/halo/missions/

  • ---- The IUSC02 TTAAii Data Designators decode (2) as: T1 (I): Observational data (Binary coded) - BUFR. T2 (U): Upper air. A1 (S): Radiosondes/pibal reports from fixed land stations(entire sounding) A2 (C): 180° - 90°E northern hemisphere. (2: Refer to WMO No.386 - Manual on the GTS - Attachment II.5) ---- Correspondence with the C13 common BUFR/CREX code table: (002/004) or (Vertical soundings (other than satellite) -- Upper-level temperature/humidity/wind reports from fixed-land stations (TEMP)) data type / data sub-type. ---- The bulletin collects reports from stations: 47102(BAENGNYEONGDO ) --- This bulletin is related with bulletin IUKC02RKSL.

  • ---- The bulletin is coded as BUFR code form: FM 94 (BUFR, Binary universal form for the representation of meteorological data) . (Refer to WMO No.306 - Manual on Codes for the definition of WMO international codes) ---- The IUCN08 TTAAii Data Designators decode (2) as: T1 (I): Observational data (Binary coded) - BUFR. T2 (U): Upper air. A1 (C): (used for single level satellite-derived reports - see Note 3) A2 (N): Northern hemisphere. (2: Refer to WMO No.386 - Manual on the GTS - Attachment II.5) ---- Correspondence with the C13 common BUFR/CREX code table: (005/000) or (Single level upper-air data (satellite) -- AMV) data type / data sub-type. ---- WMO No.9 - Volume C1 'Remarks' field: Atmospheric Motion Vectors (Infrared Channel 1) (NORTHERN HEMISPHERE); NOTE: FROM COMS (128.2° E)

  • Simulation with most recent version of MADE3 into the atmospheric chemistry general circulation model EMAC, including a detailed evaluation of a ten-year aerosol simulation with MADE3 as part of EMAC. Model details and setup specification are described in Kaiser et al. (Geosci. Model Dev., 2018). We compare simulation output to station network measurements of near-surface aerosol component mass concentrations, to airborne measurements of aerosol mass mixing ratio and number concentration vertical profiles, to ground-based and airborne measurements of particle size distributions, and to station network and satellite measurements of aerosol optical depth. Furthermore, we describe and apply a new evaluation method, which allows a comparison of model output to size-resolved electron microscopy measurements of particle composition. Although there are indications that fine mode particle deposition may be underestimated by the model, we obtained satisfactory agreement with the observations. Remaining deviations are of similar size as those identified in other global aerosol model studies. Thus, MADE3 can be considered ready for application within EMAC. Due to its detailed representation of aerosol mixing state, it is especially useful for simulating wet and dry removal of aerosol particles, aerosol-induced formation of cloud droplets and ice crystals as well as aerosol-radiation interactions. Besides studies on these fundamental processes, we also plan to use MADE3 for a reassessment of the climate effects of anthropogenic aerosol perturbations. Please cite Kaiser et al. (Geosci. Model Dev., 2018) if using the data.