Global and regional impacts of land cover changes on isoprene emissions derived from spaceborne data and the MEGAN model
Among the biogenic volatile organic compounds (BVOCs) emitted by plant foliage, isoprene is by far the most important in terms of both global emission and atmospheric impact. It is highly reactive in the air, and its degradation favours the generation of ozone (in the presence of NOx) and secondary...
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Veröffentlicht in: | Atmospheric chemistry and physics 2021-06, Vol.21 (11), p.8413-8436 |
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Zusammenfassung: | Among the biogenic volatile organic compounds (BVOCs) emitted by plant foliage, isoprene is by far the most important in terms of both global
emission and atmospheric impact. It is highly reactive in the air, and its degradation favours the generation of ozone (in the presence of
NOx) and secondary organic aerosols. A critical aspect of BVOC emission modelling is the representation of land use and land
cover (LULC). The current emission inventories are usually based on land cover maps that are either modelled and dynamic or satellite-based and
static. In this study, we use the state-of-the-art Model of Emissions of Gases and Aerosols from Nature (MEGAN) model coupled with the canopy model MOHYCAN (Model for Hydrocarbon emissions by the CANopy) to generate and evaluate emission inventories
relying on satellite-based LULC maps at annual time steps. To this purpose, we first intercompare the distribution and evolution (2001–2016) of
tree coverage from three global satellite-based datasets, MODerate resolution Imaging Spectroradiometer (MODIS), ESA Climate Change Initiative Land Cover (ESA CCI-LC), and the Global Forest Watch (GFW), and from
national inventories. Substantial differences are found between the datasets; e.g. the global areal coverage of trees ranges from 30 to
50×106 km2, with trends spanning from −0.26 to +0.03 % yr−1 between 2001 and 2016. At the national level, the increasing
trends in forest cover reported by some national inventories (in particular for the US) are contradicted by all remotely sensed datasets. To a great
extent, these discrepancies stem from the plurality of definitions of forest used. According to some local censuses, clear cut areas and seedling or
young trees are classified as forest, while satellite-based mappings of trees rely on a minimum height. Three inventories of isoprene emissions are
generated, differing only in their LULC datasets used as input: (i) the static distribution of the stand-alone version of MEGAN, (ii) the
time-dependent MODIS land cover dataset, and (iii) the MODIS dataset modified to match the tree cover distribution from the GFW database. The mean
annual isoprene emissions (350–520 Tg yr−1) span a wide range due to differences in tree distributions, especially in isoprene-rich
regions. The impact of LULC changes is a mitigating effect ranging from 0.04 to 0.33 % yr−1 on the positive trends
(0.94 % yr−1) mainly driven by temperature and solar radiation. This study highlights the uncertainty in spat |
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ISSN: | 1680-7324 1680-7316 1680-7324 |
DOI: | 10.5194/acp-21-8413-2021 |