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  • 1
    Publikationsdatum: 2020-12-18
    Beschreibung: The Arctic region plays a central role in the global climate system. Modifications in the Arctic radiative budget may strongly influence large scale atmospheric and oceanic circulation. The evaluation of the surface energy balance sensitivity to variations in several parameters, such as surface temperature, water vapour content, surface albedo, and atmospheric aerosols, is one of the main issues in assessing how the Arctic will respond to future climate changes. The NDACC station at Thule Air Base (76.5°N, 68.8°W) is equipped with a variety of instruments for the measurement of the radiative fluxes at the surface, aerosol optical properties, water vapour atmospheric content, and meteorological parameters. A Yankee Environmental System Total Solar Pyranometer (YES-TSP) and an Eppley pyrgeometer (PIR) are installed at Thule for the measurement of the global shortwave and longwave downward irradiances at the surface. The TSP was installed in 2002, while the PIR in 2009. A Cimel Sunphotometer measures aerosol optical properties and water vapour columnar content; the Cimel is part of the Aerosol Robotic Network and was installed in 2007. In winter, the water vapour columnar content is also measured at Thule with a millimeter-wave spectrometer (GBMS) operating in the 230-280 GHz range. GBMS measurements have been carried out during several winters between 2002 and 2011. A meteorological station, which measures surface temperature and pressure, relative humidity, wind speed and direction is also continuously operational at Thule. Satellite observations of the surface shortwave albedo obtained from MODIS have been used together with ground-based measurements. Four years (2007 to 2010) of surface shortwave irradiance at the surface, aerosol optical properties, and water vapour have been combined with satellite observations of the surface albedo. Radiative transfer model calculations are used to reproduce the observed shortwave fluxes and to separate the effects of the different parameters in modulating the cloud-free downward shortwave radiation at the ground. Water vapour is the main factor affecting the cloud-free shortwave irradiance at the surface. Its column value varies between 0.1 and 1.4 cm during the period spring to early autumn. Water vapour produces a reduction of the surface shortwave flux by -(212%). The surface albedo varies between 0.05 and 0.66 in the period March to September, with values larger than 0.5 in spring and smaller than 0.1 in summer. In spring the surface albedo induces an increase by +(2-4.5%) in the downward shortwave radiation. The aerosol optical depth at 500 nm is generally lower than 0.2; atmospheric aerosols produce a reduction in the shortwave radiation down to -5%. On annual base, the mean effects of water vapour and surface albedo are estimated to be –(10-11) Wm-2 and +(2-3) Wm-2, respectively. The temperature and humidity profiles in the troposphere have the strongest influence on the cloud-free downwelling longwave irradiance. In wintertime, in absence of solar radiation, the longwave fluxes dominate the surface radiation budget. GBMS water vapour measurements from winters 2009 to 2011 have been used, together with surface humidity and temperature, to investigate the relative influence of these factors in affecting the downwelling longwave irradiance.
    Beschreibung: Unpublished
    Beschreibung: Réunion Island, Francia
    Beschreibung: 1.8. Osservazioni di geofisica ambientale
    Beschreibung: 1.10. TTC - Telerilevamento
    Beschreibung: open
    Schlagwort(e): shortwave infrared ; longwave infrared ; radiation budget ; aerosols ; water vapour ; Greenland ; Arctic ; 01. Atmosphere::01.01. Atmosphere::01.01.05. Radiation
    Repository-Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Materialart: Conference paper
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    Publikationsdatum: 2020-12-18
    Beschreibung: Several instruments are operational at Thule Air Base (76.5oN, 68.8oW) as part of the Network for Detection of Atmospheric Composition Change. A lidar was installed in 1990 and has been operational particularly during the winter season. Lidar measurements are used to derive the aerosol backscatter ratio between about 10 and 35 km, and the atmospheric temperature (T) profile from 25 up to 70 km, with a resolution of 150 m. A ground-based millimeter-wave spectrometer (GBMS) was installed at Thule in 2001, and has been operational during the winter seasons of 2001-2003 and 2009-2011. The GBMS permits to derive the atmospheric concentration profiles of different chemical species, such as O3, CO, N2O, and HNO3, between about 15 and 80 km at a resolution of 6-8 km. The Arctic winter stratosphere is characterized by a high variability, and detection of trends is particularly difficult. The evolution of the vortex and the temperatures in the lower stratosphere has a large impact on formation of Polar Stratospheric Clouds (PSC) and on the stratosphere chemical evolution. Coldest winters occurred in 1999-2000, and 2004-2005. Intensive measurement campaigns were conducted at Thule Air Base during winters 2008-2009 and 2010-2011. These two winters have been deeply different in their thermal, dynamical and chemical evolution. The 2008-2009 Arctic winter has been characterized by the most intense Sudden Stratospheric Warming (SSW) event ever observed, and the maximum of this warming was detected over Greenland. Thus, ground-based observations of the thermal structure and chemical composition of the middle atmosphere from the station at Thule Air Base have permitted to show the evolution of the phenomenon and its interactions with the dynamical structure of the polar vortex in the region of maximum warming. On the contrary, the 2010-2011 has been a very cold winter, and polar stratospheric clouds have been detected by lidar from mid-February to mid-March at Thule Air Base. This very cold winter, together with the massive formation of PSCs, has caused the record stratospheric ozone loss that is occurring in spring 2011 in the Arctic. In this study, we will present a summary of the measurements of the thermal and chemical stratospheric structure obtained at Thule Air Base between 1990 and 2011, with special attention to the two winters of 2008-2009 and 2010-2011.
    Beschreibung: Unpublished
    Beschreibung: Sheraton Denver Downtown Hotel, Denver, CO, USA
    Beschreibung: 1.8. Osservazioni di geofisica ambientale
    Beschreibung: 1.10. TTC - Telerilevamento
    Beschreibung: 3.7. Dinamica del clima e dell'oceano
    Beschreibung: open
    Schlagwort(e): stratospheric composition ; ozone ; nitric acid ; sudden stratospheric warming ; Greenland ; Arctic ozone loss ; lidar observations ; microwave remote sensing ; 01. Atmosphere::01.01. Atmosphere::01.01.99. General or miscellaneous ; 01. Atmosphere::01.01. Atmosphere::01.01.01. Composition and Structure
    Repository-Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Materialart: Abstract
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
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