Spatial variation of modelled total, dry and wet nitrogen deposition to forests at global scale

被引:81
作者
Schwede, Donna B. [1 ]
Simpson, David [2 ,3 ]
Tan, Jiani [4 ]
Fu, Joshua S. [4 ]
Dentener, Frank [5 ]
Du, Enzai [6 ,7 ]
deVries, Wim [8 ,9 ]
机构
[1] US EPA, Natl Exposure Res Lab, Res Triangle Pk, NC 27717 USA
[2] Norwegian Meteorol Inst, EMEP MSC W, Oslo, Norway
[3] Chalmers Univ Technol, Dept Space Earth & Environm, Gothenburg, Sweden
[4] Univ Tennessee, Dept Civil & Environm Engn, Knoxville, TN 37996 USA
[5] European Commiss, Joint Res Ctr, Ispra, Italy
[6] Beijing Normal Univ, Fac Geog Sci, State Key Lab Earth Surface Proc & Resource Ecol, Beijing 100875, Peoples R China
[7] Beijing Normal Univ, Fac Geog Sci, Sch Nat Resources, Beijing 100875, Peoples R China
[8] Wageningen Univ & Res, Environm Res, POB 47, NL-6700 AA Wageningen, Netherlands
[9] Wageningen Univ & Res, Environm Syst Anal Grp, POB 47, NL-6700 AA Wageningen, Netherlands
基金
欧盟地平线“2020”;
关键词
Nitrogen deposition; Dry deposition; Wet deposition; Forest biomes; Modelling approach; CHEMICAL-TRANSPORT MODEL; AIR-QUALITY MODEL; CARBON SEQUESTRATION; INORGANIC NITROGEN; ATMOSPHERIC DEPOSITION; UNCERTAINTY ASSESSMENT; VEGETATIVE CANOPIES; PARTICLE DEPOSITION; REACTIVE NITROGEN; FLOOR VEGETATION;
D O I
10.1016/j.envpol.2018.09.084
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Forests are an important biome that covers about one third of the global land surface and provides important ecosystem services. Since atmospheric deposition of nitrogen (N) can have both beneficial and deleterious effects, it is important to quantify the amount of N deposition to forest ecosystems. Measurements of N deposition to the numerous forest biomes across the globe are scarce, so chemical transport models are often used to provide estimates of atmospheric N inputs to these ecosystems. We provide an overview of approaches used to calculate N deposition in commonly used chemical transport models. The Task Force on Hemispheric Transport of Air Pollution (HTAP2) study intercompared N deposition values from a number of global chemical transport models. Using a multi-model mean calculated from the HTAP2 deposition values, we map N deposition to global forests to examine spatial variations in total, dry and wet deposition. Highest total N deposition occurs in eastern and southern China, Japan, Eastern U.S. and Europe while the highest dry deposition occurs in tropical forests. The European Monitoring and Evaluation Program (EMEP) model predicts grid-average deposition, but also produces deposition by land use type allowing us to compare deposition specifically to forests with the grid-average value. We found that, for this study, differences between the grid-average and forest specific could be as much as a factor of two and up to more than a factor of five in extreme cases. This suggests that consideration should be given to using forest-specific deposition for input to ecosystem assessments such as critical loads determinations. Published by Elsevier Ltd.
引用
收藏
页码:1287 / 1301
页数:15
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