@InCollection{AasCAABBCDDDDDDFGGHIKKKLLPPPRSSTVV:2014:PrNiDe,
author = "Aas, W. and Carou, S. and Alebic-Juretic, A. and Aneja, V. P and
Balasubramanian, R and Berge, H. and Cape, J. N. and Delon, C. and
Denmead, O. T. and Dennis, R. L. and Dentener, F. and Dore, A. J.
and Du, E. and Forti, Maria Cristina and Galy-Lacaux, C. and
Geupel, Markus and Haeuber, Richard and Iacoban, Carmen and
Komarov, Alexander S. and Kubin, Eero and Kulshrestha, Umesh C.
and Lamb, Brian and Liu, Xuejun and Patra, D. D. and Pienaar,
Jacobus J. and Pinho, Pedro and Rao, P. S. P. and Shen, Jianlin
and Sutton, Mark A. and Theobald, Mark R. and Vadrevu, Krishna P.
and Vet, Robert",
title = "Progress in Nitrogen Deposition Monitoring and Modelling",
booktitle = "Nitrogen Deposition, Critical Loads and Biodiversity",
publisher = "Springer",
year = "2014",
editor = "Sutton, M. A. and Mason, K. E. and Sheppard, L. J. and Sverdrup,
H. and Haeuber, R. and Hicks, W. K.",
pages = "455--463",
address = "Berlin",
keywords = "nitrogen, inorganic, modelling, organic, wet and dry deposition.",
abstract = "The chapter reviews progress in monitoring and modelling of
atmospheric nitrogen (N) deposition at regional and global scales.
The Working Group expressed confidence in the inorganic N wet
deposition estimates in U.S., eastern Canada, Europe and parts of
East Asia. But, long-term wet or dry N deposition information in
large parts of Asia, South America, parts of Africa,
Australia/Oceania, and oceans and coastal areas is lacking.
Presently, robust estimates are only available for inorganic N as
existing monitoring generally does not measure the complete suite
of N species, impeding the closing of the atmospheric N budget.
The most important species not routinely measured are nitrogen
dioxide (NO2), ammonia (NH3), organic N and nitric acid (HNO3).
Uncertainty is much higher in dry deposition than in wet
deposition estimates. Inferential modelling (combining air
concentrations with exchange rates) and direct flux measurements
are good tools to estimate dry deposition; however, they are not
widely applied. There is a lack of appropriate parameterizations
for different land uses and compounds for input into inferential
models. There is also a lack of direct dry deposition flux
measurements to test inferential models and atmospheric model
estimates.",
affiliation = "{} and {} and {} and {} and {} and {} and {} and {} and {} and {}
and {} and {} and {} and {Instituto Nacional de Pesquisas
Espaciais (INPE)}",
label = "self-archiving-INPE-MCTI-GOV-BR",
language = "en",
targetfile = "N-Deposit-Chap48.pdf",
urlaccessdate = "27 abr. 2024"
}