Impacts of climate and emission changes on nitrogen deposition in Europe: a multi-model study

被引:89
作者
Simpson, D. [1 ,2 ]
Andersson, C. [3 ]
Christensen, J. H. [4 ]
Engardt, M. [3 ]
Geels, C. [4 ]
Nyiri, A. [1 ]
Posch, M. [5 ]
Soares, J. [6 ]
Sofiev, M. [6 ]
Wind, P. [1 ,7 ]
Langner, J. [3 ]
机构
[1] EMEP MSC W, Norwegian Meteorol Inst, Oslo, Norway
[2] Chalmers Univ Technol, Dept Earth & Space Sci, S-41296 Gothenburg, Sweden
[3] Swedish Meteorol & Hydrol Inst, S-60176 Norrkoping, Sweden
[4] Aarhus Univ, Dept Environm Sci, DK-4000 Roskilde, Denmark
[5] Natl Inst Publ Hlth & Environm RIVM, Bilthoven, Netherlands
[6] Finnish Meteorol Inst, FIN-00101 Helsinki, Finland
[7] Univ Tromso, N-9037 Tromso, Norway
关键词
GAS-PARTICLE INTERACTIONS; AIR-POLLUTION LEVELS; OZONE DEPOSITION; SURFACE OZONE; REDUCTION AGREEMENTS; ATMOSPHERIC AMMONIA; REACTIVE NITROGEN; MODEL DESCRIPTION; DUTCH HEATHLAND; DRY DEPOSITION;
D O I
10.5194/acp-14-6995-2014
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The impact of climate and emissions changes on the deposition of reactive nitrogen (Nr) over Europe was studied using four offline regional chemistry transport models (CTMs) driven by the same global projection of future climate over the period 2000-2050. Anthropogenic emissions for the years 2005 and 2050 were used for simulations of both present and future periods in order to isolate the impact of climate change, hemispheric boundary conditions and emissions, and to assess the robustness of the results across the different models. The results from these four CTMs clearly show that the main driver of future N-deposition changes is the specified emission change. Under the specified emission scenario for 2050, emissions of oxidised nitrogen were reduced substantially, whereas emissions of NH3 increase to some extent, and these changes are largely reflected in the modelled concentrations and depositions. The lack of sulfur and oxidised nitrogen in the future atmosphere results in a much larger fraction of NHx being present in the form of gaseous ammonia. Predictions for wet and total deposition were broadly consistent, although the three fine-scale models resolve European emission areas and changes better than the hemisphericscale model. The biggest difference in the models is for predictions of individual N compounds. One model (EMEP) was used to explore changes in critical loads, also in conjunction with speculative climate-induced increases in NH3 emissions. These calculations suggest that the area of ecosystems that exceeds critical loads is reduced from 64% for year 2005 emissions levels to 50% for currently estimated 2050 levels. A possible climate-induced increase in NH3 emissions could worsen the situation, with areas exceeded increasing again to 57% (for a 30% NH3 emission increase).
引用
收藏
页码:6995 / 7017
页数:23
相关论文
共 119 条
[1]   Lessons learnt from the first EMEP intensive measurement periods [J].
Aas, W. ;
Tsyro, S. ;
Bieber, E. ;
Bergstrom, R. ;
Ceburnis, D. ;
Ellermann, T. ;
Fagerli, H. ;
Froelich, M. ;
Gehrig, R. ;
Makkonen, U. ;
Nemitz, E. ;
Otjes, R. ;
Perez, N. ;
Perrino, C. ;
Prevot, A. S. H. ;
Putaud, J. -P. ;
Simpson, D. ;
Spindler, G. ;
Vana, M. ;
Yttri, K. E. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2012, 12 (17) :8073-8094
[2]   Regional and Global Emissions of Air Pollutants: Recent Trends and Future Scenarios [J].
Amann, Markus ;
Klimont, Zbigniew ;
Wagner, Fabian .
ANNUAL REVIEW OF ENVIRONMENT AND RESOURCES, VOL 38, 2013, 38 :31-55
[3]  
Andersson C, 2007, TELLUS B, V59, P77, DOI [10.1111/j.1600-0889.2006.00196.x, 10.1111/j.1600-0889.2006.00231.x]
[4]   European ozone in a future climate: Importance of changes in dry deposition and isoprene emissions [J].
Andersson, Camilla ;
Engardt, Magnuz .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2010, 115
[5]  
[Anonymous], 1 TSAP IIASA
[6]  
[Anonymous], EUROPEAN NITROGEN AS
[7]  
[Anonymous], [No title captured], DOI DOI 10.1023/A:1013131927678)
[8]  
Asman W. A. H., 1994, MARINE RES, V35
[9]   Evaluation of a regional air-quality model with bidirectional NH3 exchange coupled to an agroecosystem model [J].
Bash, J. O. ;
Cooter, E. J. ;
Dennis, R. L. ;
Walker, J. T. ;
Pleim, J. E. .
BIOGEOSCIENCES, 2013, 10 (03) :1635-1645
[10]  
Bergstrom R, 1998, 82 RMK SWED MET HYDR