Predicting Acidification Recovery at the Hubbard Brook Experimental Forest, New Hampshire: Evaluation of Four Models
(2010) In Environmental Science & Technology 44(23). p.9003-9009- Abstract
- The performance and prediction uncertainty (owing to parameter and structural uncertainties) of four dynamic watershed acidification models (MAGIC, PnET-BGC, SAFE, and VSD) were assessed by systematically applying them to data from the Hubbard Brook Experimental Forest (HBEF), New Hampshire, where long-term records of precipitation and stream chemistry were available. In order to facilitate systematic evaluation, Monte Carlo simulation was used to randomly generate common model input data sets (n ) 10 000) from parameter distributions; input data were subsequently translated among models to retain consistency. The model simulations were objectively calibrated against observed data (streamwater: 1963-2004, soil: 1983). The ensemble of... (More)
- The performance and prediction uncertainty (owing to parameter and structural uncertainties) of four dynamic watershed acidification models (MAGIC, PnET-BGC, SAFE, and VSD) were assessed by systematically applying them to data from the Hubbard Brook Experimental Forest (HBEF), New Hampshire, where long-term records of precipitation and stream chemistry were available. In order to facilitate systematic evaluation, Monte Carlo simulation was used to randomly generate common model input data sets (n ) 10 000) from parameter distributions; input data were subsequently translated among models to retain consistency. The model simulations were objectively calibrated against observed data (streamwater: 1963-2004, soil: 1983). The ensemble of calibrated models was used to assess future response of soil and stream chemistry to reduced sulfur deposition at the HBEF. Although both hindcast (1850-1962) and forecast (2005-2100) predictions were qualitatively similar across the four models, the temporal pattern of key indicators of acidification recovery (stream acid neutralizing capacity and soil base saturation) differed substantially. The range in predictions resulted from differences in model structure and their associated posterior parameter distributions. These differences can be accommodated by employing multiple models (ensemble analysis) but have implications for individual model applications. (Less)
Please use this url to cite or link to this publication:
https://lup.lub.lu.se/record/1710052
- author
- Tominaga, Koji
; Aherne, Julian
; Watmough, Shaun A.
; Alveteg, Mattias
LU
; Cosby, Bernard J. ; Driscoll, Charles T. ; Posch, Maximilian and Pourmokhtarian, Afshin
- organization
- publishing date
- 2010
- type
- Contribution to journal
- publication status
- published
- subject
- in
- Environmental Science & Technology
- volume
- 44
- issue
- 23
- pages
- 9003 - 9009
- publisher
- The American Chemical Society (ACS)
- external identifiers
-
- pmid:21028800
- wos:000284523400035
- scopus:78650291124
- pmid:21028800
- ISSN
- 1520-5851
- DOI
- 10.1021/es102243j
- language
- English
- LU publication?
- yes
- additional info
- Publication Date (Web): October 28, 2010
- id
- 2962336e-3e88-4262-bb15-bfb931cb9ade (old id 1710052)
- date added to LUP
- 2016-04-01 11:07:28
- date last changed
- 2025-04-04 14:54:36
@article{2962336e-3e88-4262-bb15-bfb931cb9ade, abstract = {{The performance and prediction uncertainty (owing to parameter and structural uncertainties) of four dynamic watershed acidification models (MAGIC, PnET-BGC, SAFE, and VSD) were assessed by systematically applying them to data from the Hubbard Brook Experimental Forest (HBEF), New Hampshire, where long-term records of precipitation and stream chemistry were available. In order to facilitate systematic evaluation, Monte Carlo simulation was used to randomly generate common model input data sets (n ) 10 000) from parameter distributions; input data were subsequently translated among models to retain consistency. The model simulations were objectively calibrated against observed data (streamwater: 1963-2004, soil: 1983). The ensemble of calibrated models was used to assess future response of soil and stream chemistry to reduced sulfur deposition at the HBEF. Although both hindcast (1850-1962) and forecast (2005-2100) predictions were qualitatively similar across the four models, the temporal pattern of key indicators of acidification recovery (stream acid neutralizing capacity and soil base saturation) differed substantially. The range in predictions resulted from differences in model structure and their associated posterior parameter distributions. These differences can be accommodated by employing multiple models (ensemble analysis) but have implications for individual model applications.}}, author = {{Tominaga, Koji and Aherne, Julian and Watmough, Shaun A. and Alveteg, Mattias and Cosby, Bernard J. and Driscoll, Charles T. and Posch, Maximilian and Pourmokhtarian, Afshin}}, issn = {{1520-5851}}, language = {{eng}}, number = {{23}}, pages = {{9003--9009}}, publisher = {{The American Chemical Society (ACS)}}, series = {{Environmental Science & Technology}}, title = {{Predicting Acidification Recovery at the Hubbard Brook Experimental Forest, New Hampshire: Evaluation of Four Models}}, url = {{http://dx.doi.org/10.1021/es102243j}}, doi = {{10.1021/es102243j}}, volume = {{44}}, year = {{2010}}, }