Potential effects of changes in precipitation and temperature on wet deposition in central Pennsylvania

Anthony Buda, David R. DeWalle

Research output: Contribution to journalArticle

9 Citations (Scopus)

Abstract

Changes in regional climate can alter conditions that control the transport, chemical transformation, and eventual deposition of atmospheric pollutants. In Pennsylvania, climate change is projected to increase mean annual temperatures by 4°C and annual precipitation amounts by about 5% through 2100. The objective of this study was to determine how increases in temperature and precipitation would affect concentrations and wet deposition of SO42-, NO3-, NH4+, and H+ ions at a National Atmospheric Deposition Program site (NADP, PA15) in central Pennsylvania. Event-based wet deposition data were obtained from the Multi-State Atmospheric Power Production Pollution Study (MAP3S) monitoring program for the period 1976-1989. Forward stepwise regression was used to predict log-normal concentrations per event using mean temperature, precipitation, Julian Date, and interactions of temperature and precipitation with Julian Date as predictor variables. Julian Date was included to adjust for time trends in precipitation chemistry and climate data. Results were categorized by annual periods, growing season/dormant season, and synoptic climate types. Significant positive effects of temperature on concentration and deposition were found for SO42-, NH4+, and H+ but not for NO3-. Precipitation increases reduced the concentration of each ion due to dilution, but the lower concentration only minimally offset the increase in wet deposition due to the increased precipitation. The effects of climate change during the growing season (April-September) were projected to cause greater increases in the magnitude of SO42-, NO3-, and H+ concentrations and wet deposition than in the dormant season (October-March). Ammonium (NH4+) increases were greatest during the dormant season. Climate change effects on wet deposition were generally similar among synoptic climate types with the greatest effects occurring for cold fronts and warm fronts. The impacts of climate change for this central PA site could increase overall annual wet deposition of SO42- by up to 29%, NO3- by up to 6%, NH4+ by up to 23%, and H+ by up to 17% through the year 2100, assuming that the statistical relationships hold true and that no changes in the emission of these ions occur.

Original languageEnglish (US)
Pages (from-to)3767-3778
Number of pages12
JournalAtmospheric Environment
Volume36
Issue number23
DOIs
StatePublished - Aug 1 2002

Fingerprint

wet deposition
Climate change
climate change
temperature
Temperature
ion
growing season
warm front
precipitation (chemistry)
cold front
Ions
atmospheric deposition
regional climate
effect
dilution
atmospheric pollution
ammonium
Precipitation (meteorology)
pollution
Dilution

All Science Journal Classification (ASJC) codes

  • Atmospheric Science
  • Environmental Science(all)
  • Pollution

Cite this

@article{9f9cdbd98bac4870a53612e67080681a,
title = "Potential effects of changes in precipitation and temperature on wet deposition in central Pennsylvania",
abstract = "Changes in regional climate can alter conditions that control the transport, chemical transformation, and eventual deposition of atmospheric pollutants. In Pennsylvania, climate change is projected to increase mean annual temperatures by 4°C and annual precipitation amounts by about 5{\%} through 2100. The objective of this study was to determine how increases in temperature and precipitation would affect concentrations and wet deposition of SO42-, NO3-, NH4+, and H+ ions at a National Atmospheric Deposition Program site (NADP, PA15) in central Pennsylvania. Event-based wet deposition data were obtained from the Multi-State Atmospheric Power Production Pollution Study (MAP3S) monitoring program for the period 1976-1989. Forward stepwise regression was used to predict log-normal concentrations per event using mean temperature, precipitation, Julian Date, and interactions of temperature and precipitation with Julian Date as predictor variables. Julian Date was included to adjust for time trends in precipitation chemistry and climate data. Results were categorized by annual periods, growing season/dormant season, and synoptic climate types. Significant positive effects of temperature on concentration and deposition were found for SO42-, NH4+, and H+ but not for NO3-. Precipitation increases reduced the concentration of each ion due to dilution, but the lower concentration only minimally offset the increase in wet deposition due to the increased precipitation. The effects of climate change during the growing season (April-September) were projected to cause greater increases in the magnitude of SO42-, NO3-, and H+ concentrations and wet deposition than in the dormant season (October-March). Ammonium (NH4+) increases were greatest during the dormant season. Climate change effects on wet deposition were generally similar among synoptic climate types with the greatest effects occurring for cold fronts and warm fronts. The impacts of climate change for this central PA site could increase overall annual wet deposition of SO42- by up to 29{\%}, NO3- by up to 6{\%}, NH4+ by up to 23{\%}, and H+ by up to 17{\%} through the year 2100, assuming that the statistical relationships hold true and that no changes in the emission of these ions occur.",
author = "Anthony Buda and DeWalle, {David R.}",
year = "2002",
month = "8",
day = "1",
doi = "10.1016/S1352-2310(02)00223-6",
language = "English (US)",
volume = "36",
pages = "3767--3778",
journal = "Atmospheric Environment",
issn = "1352-2310",
publisher = "Elsevier Limited",
number = "23",

}

Potential effects of changes in precipitation and temperature on wet deposition in central Pennsylvania. / Buda, Anthony; DeWalle, David R.

In: Atmospheric Environment, Vol. 36, No. 23, 01.08.2002, p. 3767-3778.

Research output: Contribution to journalArticle

TY - JOUR

T1 - Potential effects of changes in precipitation and temperature on wet deposition in central Pennsylvania

AU - Buda, Anthony

AU - DeWalle, David R.

PY - 2002/8/1

Y1 - 2002/8/1

N2 - Changes in regional climate can alter conditions that control the transport, chemical transformation, and eventual deposition of atmospheric pollutants. In Pennsylvania, climate change is projected to increase mean annual temperatures by 4°C and annual precipitation amounts by about 5% through 2100. The objective of this study was to determine how increases in temperature and precipitation would affect concentrations and wet deposition of SO42-, NO3-, NH4+, and H+ ions at a National Atmospheric Deposition Program site (NADP, PA15) in central Pennsylvania. Event-based wet deposition data were obtained from the Multi-State Atmospheric Power Production Pollution Study (MAP3S) monitoring program for the period 1976-1989. Forward stepwise regression was used to predict log-normal concentrations per event using mean temperature, precipitation, Julian Date, and interactions of temperature and precipitation with Julian Date as predictor variables. Julian Date was included to adjust for time trends in precipitation chemistry and climate data. Results were categorized by annual periods, growing season/dormant season, and synoptic climate types. Significant positive effects of temperature on concentration and deposition were found for SO42-, NH4+, and H+ but not for NO3-. Precipitation increases reduced the concentration of each ion due to dilution, but the lower concentration only minimally offset the increase in wet deposition due to the increased precipitation. The effects of climate change during the growing season (April-September) were projected to cause greater increases in the magnitude of SO42-, NO3-, and H+ concentrations and wet deposition than in the dormant season (October-March). Ammonium (NH4+) increases were greatest during the dormant season. Climate change effects on wet deposition were generally similar among synoptic climate types with the greatest effects occurring for cold fronts and warm fronts. The impacts of climate change for this central PA site could increase overall annual wet deposition of SO42- by up to 29%, NO3- by up to 6%, NH4+ by up to 23%, and H+ by up to 17% through the year 2100, assuming that the statistical relationships hold true and that no changes in the emission of these ions occur.

AB - Changes in regional climate can alter conditions that control the transport, chemical transformation, and eventual deposition of atmospheric pollutants. In Pennsylvania, climate change is projected to increase mean annual temperatures by 4°C and annual precipitation amounts by about 5% through 2100. The objective of this study was to determine how increases in temperature and precipitation would affect concentrations and wet deposition of SO42-, NO3-, NH4+, and H+ ions at a National Atmospheric Deposition Program site (NADP, PA15) in central Pennsylvania. Event-based wet deposition data were obtained from the Multi-State Atmospheric Power Production Pollution Study (MAP3S) monitoring program for the period 1976-1989. Forward stepwise regression was used to predict log-normal concentrations per event using mean temperature, precipitation, Julian Date, and interactions of temperature and precipitation with Julian Date as predictor variables. Julian Date was included to adjust for time trends in precipitation chemistry and climate data. Results were categorized by annual periods, growing season/dormant season, and synoptic climate types. Significant positive effects of temperature on concentration and deposition were found for SO42-, NH4+, and H+ but not for NO3-. Precipitation increases reduced the concentration of each ion due to dilution, but the lower concentration only minimally offset the increase in wet deposition due to the increased precipitation. The effects of climate change during the growing season (April-September) were projected to cause greater increases in the magnitude of SO42-, NO3-, and H+ concentrations and wet deposition than in the dormant season (October-March). Ammonium (NH4+) increases were greatest during the dormant season. Climate change effects on wet deposition were generally similar among synoptic climate types with the greatest effects occurring for cold fronts and warm fronts. The impacts of climate change for this central PA site could increase overall annual wet deposition of SO42- by up to 29%, NO3- by up to 6%, NH4+ by up to 23%, and H+ by up to 17% through the year 2100, assuming that the statistical relationships hold true and that no changes in the emission of these ions occur.

UR - http://www.scopus.com/inward/record.url?scp=0036695925&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=0036695925&partnerID=8YFLogxK

U2 - 10.1016/S1352-2310(02)00223-6

DO - 10.1016/S1352-2310(02)00223-6

M3 - Article

AN - SCOPUS:0036695925

VL - 36

SP - 3767

EP - 3778

JO - Atmospheric Environment

JF - Atmospheric Environment

SN - 1352-2310

IS - 23

ER -