16 resultados para University of Melbourne
Resumo:
Wollongong, Australia is an urban site at the intersection of anthropogenic, biomass burning, biogenic and marine sources of atmospheric trace gases. The location offers a valuable opportunity to study drivers of atmospheric composition in the Southern Hemisphere. Here, a record of surface carbon monoxide (CO), methane (CH4) and carbon dioxide (CO2) was measured with an in situ Fourier transform infrared trace gas analyser between April 2011 and August 2014. Clean air was found to arrive at Wollongong in approximately 10% of air masses. Biomass burning influence was evident in the average annual cycle of clean air CO during austral spring. A significant negative short-term trend was found in clean air CO (-1.5 nmol/mol/a), driven by a reduction in northern Australian biomass burning. Significant short-term positive trends in clean air CH4 (5.4 nmol/mol/a) and CO2 (1.9 ?mol/mol/a) were consistent with the long-term global average trends. Polluted Wollongong air was investigated using wind-direction/wind-speed clustering, which revealed major influence from local urban and industrial sources from the south. High values of CH4, with anthropogenic DCH4/DCO2 enhancement ratio signatures, originated from the northwest, in the direction of local coal mining. A pollution climatology was developed for the region using back trajectory analysis and DO3/DCO enhancement ratios. Ozone production environments in austral spring and summer were associated with anticyclonic meteorology on the east coast of Australia, while ozone depletion environments in autumn and winter were associated with continental transport, or fast moving trajectories from southern latitudes. This implies the need to consider meteorological conditions when developing policies for controlling air quality.
Continuous meteorological observations in high-resolution (1Hz) at University of Oldenburg (2014-02)
Continuous meteorological observations in high-resolution (1Hz) at University of Oldenburg (2014-10)
Continuous meteorological observations in high-resolution (1Hz) at University of Oldenburg (2014-01)
Continuous meteorological observations in high-resolution (1Hz) at University of Oldenburg (2014-05)
Continuous meteorological observations in high-resolution (1Hz) at University of Oldenburg (2014-12)
Continuous meteorological observations in high-resolution (1Hz) at University of Oldenburg (2014-04)
Continuous meteorological observations in high-resolution (1Hz) at University of Oldenburg (2014-11)
Continuous meteorological observations in high-resolution (1Hz) at University of Oldenburg (2014-08)
Resumo:
The importance of pollen analytical data for the reconstruction of the natural conditions and their changes caused by human impact in prehistorical and historical times is beyond all doubt. Pollen analysis can, however, be hampered by poor pollen preservation and low pollen concentrations. As an example pollen assemblages from excavation areas near Pompeii (see doi:10.1594/PANGAEA.777531) and from the Old Botanical Garden of the University of Göttingen are discussed. A pollen diagram (see doi:10.1594/PANGAEA.820590) from the site Höllerer See in Austria (N of the city of Salzburg) demonstrates the intensive agricultural influence on the vegetation of the area during Roman and Medieval times. Human influence was much weaker during the Iron and the Bronze ages. There is no indication of human impact on the vegetation during the Migration period.
Continuous meteorological observations in high-resolution (1Hz) at University of Oldenburg (2014-06)
Continuous meteorological observations in high-resolution (1Hz) at University of Oldenburg (2014-03)