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M ALTAF ARAIN

Biographic Data

ID5246111
NAMEM ALTAF ARAIN
GIVEN NAMESM ALTAF
FAMILY NAMEARAIN
SIGNATUREARAIN M A
AFFILIATIONSMcMaster University
ORCID0000-0002-1433-5173
VERIFIEDYes
TOTAL WORKS8
TOTAL CITATIONS0
AUTHOR COUNT8
EDITOR COUNT0
FIRST PUBLICATION YEAR2005
LATEST PUBLICATION YEAR2023
H-INDEX0
  • Revealing how intra- and inter-annual variability of carbon uptake (GPP) affects wood cell biomass in an eastern white pine forest

    Open Access•Paulina F Puchi, Myroslava Khomik et al.•ARTICLE•Environmental Research Letters•2023

    Forests are major terrestrial carbon (C) sinks and play a crucial role in climate change mitigation. Despite extensive studies on forest C sequestration, the relationship between seasonal C uptake and its allocation to woody biomass is poorly understood. Here we used a novel dendro-anatomical approach to investigate the relationships between climate variability, C uptake, and woody biomass growth in an 80 year-old eastern white pine ( Pinus strob…

  • Stomatal response to decreased relative humidity constrains the acceleration of terrestrial evapotranspiration

    Open Access•Mingzhong Xiao, Zhongbo Yu et al.•ARTICLE•Environmental Research Letters•2020

    Terrestrial evapotranspiration (ET) is thermodynamically expected to increase with increasing atmospheric temperature; however, the actual constraints on the intensification of ET remain uncertain due to a lack of direct observations. Based on the FLUXNET2015 Dataset, we found that relative humidity (RH) is a more important driver of ET than temperature. While actual ET decrease at reduced RH, potential ET increases, consistently with the complem…

  • Quantifying the effect of forest age in annual net forest carbon balance

    Open Access•Simon Besnard, Nuno Carvalhais et al.•ARTICLE•Environmental Research Letters•2018

    Forests dominate carbon (C) exchanges between the terrestrial biosphere and the atmosphere on land. In the long term, the net carbon flux between forests and the atmosphere has been significantly impacted by changes in forest cover area and structure due to ecological disturbances and management activities. Current empirical approaches for estimating net ecosystem productivity (NEP) rarely consider forest age as a predictor, which represents vari…

  • Disentangling climatic and anthropogenic controls on global terrestrial evapotranspiration trends

    Open Access•Jiafu Mao, Wenting Fu et al.•ARTICLE•Environmental Research Letters•2015

    We examined natural and anthropogenic controls on terrestrial evapotranspiration (ET) changes from 1982 to 2010 using multiple estimates from remote sensing-based datasets and process-oriented land surface models. A significant increasing trend of ET in each hemisphere was consistently revealed by observationally-constrained data and multi-model ensembles that considered historic natural and anthropogenic drivers. The climate impacts were simulat…

  • Terrestrial Gross Carbon Dioxide Uptake: Global Distribution and Covariation with Climate

    Open Access•Christian Beer, Markus Reichstein et al.•ARTICLE•Science•2010

    Carbon Cycle and Climate Change As climate change accelerates, it is important to know the likely impact of climate change on the carbon cycle (see the Perspective by Reich ). Gross primary production (GPP) is a measure of the amount of CO 2 removed from the atmosphere every year to fuel photosynthesis. Beer et al. (p. 834 , published online 5 July) used a combination of observation and calculation to estimate that the total GPP by terrestrial pl…

  • Climate control of terrestrial carbon exchange across biomes and continents

    Open Access•Chuixiang Yi, Daniel Ricciuto et al.•ARTICLE•Environmental Research Letters•2010

    Understanding the relationships between climate and carbon exchange by terrestrial ecosystems \nis critical to predict future levels of atmospheric carbon dioxide because of the potential \naccelerating effects of positive climate–carbon cycle feedbacks. However, directly observed \nrelationships between climate and terrestrial CO2 exchange with the atmosphere across biomes \nand continents are lacking. Here we present data describing the relatio…

  • Meteorological influences on the spatial and temporal variability of NO 2 in Toronto and Hamilton

    Open Access•M ALTAF ARAIN, ROSE BLAIR et al.•ARTICLE•Canadian Geographies /…•2009•References: 42

    The spatial and temporal variability of nitrogen dioxide (NO 2 ) concentrations and their relationships with meteorology was evaluated in the Toronto–Hamilton urban airshed. NO 2 concentrations were highest in the early morning and late evening. Mean concentrations were highest in winter, although individual one‐hour NO 2 concentrations were found to be highest in summer. Wind direction was the strongest control on hourly NO 2 concentration, and …

  • A review and evaluation of intraurban air pollution exposure models

    Open Access•Michael Jerrett, M ALTAF ARAIN et al.•ARTICLE•Journal of Exposure Science &…•2005

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  • A review and evaluation of intraurban air pollution exposure models

    Open Access•Michael Jerrett, M ALTAF ARAIN et al.•ARTICLE•Journal of Exposure Science &…•2005

  • Meteorological influences on the spatial and temporal variability of NO 2 in Toronto and Hamilton

    Open Access•M ALTAF ARAIN, ROSE BLAIR et al.•ARTICLE•Canadian Geographies /…•2009•References: 42

    The spatial and temporal variability of nitrogen dioxide (NO 2 ) concentrations and their relationships with meteorology was evaluated in the Toronto–Hamilton urban airshed. NO 2 concentrations were highest in the early morning and late evening. Mean concentrations were highest in winter, although individual one‐hour NO 2 concentrations were found to be highest in summer. Wind direction was the strongest control on hourly NO 2 concentration, and …

  • Terrestrial Gross Carbon Dioxide Uptake: Global Distribution and Covariation with Climate

    Open Access•Christian Beer, Markus Reichstein et al.•ARTICLE•Science•2010

    Carbon Cycle and Climate Change As climate change accelerates, it is important to know the likely impact of climate change on the carbon cycle (see the Perspective by Reich ). Gross primary production (GPP) is a measure of the amount of CO 2 removed from the atmosphere every year to fuel photosynthesis. Beer et al. (p. 834 , published online 5 July) used a combination of observation and calculation to estimate that the total GPP by terrestrial pl…

  • Climate control of terrestrial carbon exchange across biomes and continents

    Open Access•Chuixiang Yi, Daniel Ricciuto et al.•ARTICLE•Environmental Research Letters•2010

    Understanding the relationships between climate and carbon exchange by terrestrial ecosystems \nis critical to predict future levels of atmospheric carbon dioxide because of the potential \naccelerating effects of positive climate–carbon cycle feedbacks. However, directly observed \nrelationships between climate and terrestrial CO2 exchange with the atmosphere across biomes \nand continents are lacking. Here we present data describing the relatio…

  • Disentangling climatic and anthropogenic controls on global terrestrial evapotranspiration trends

    Open Access•Jiafu Mao, Wenting Fu et al.•ARTICLE•Environmental Research Letters•2015

    We examined natural and anthropogenic controls on terrestrial evapotranspiration (ET) changes from 1982 to 2010 using multiple estimates from remote sensing-based datasets and process-oriented land surface models. A significant increasing trend of ET in each hemisphere was consistently revealed by observationally-constrained data and multi-model ensembles that considered historic natural and anthropogenic drivers. The climate impacts were simulat…

  • Quantifying the effect of forest age in annual net forest carbon balance

    Open Access•Simon Besnard, Nuno Carvalhais et al.•ARTICLE•Environmental Research Letters•2018

    Forests dominate carbon (C) exchanges between the terrestrial biosphere and the atmosphere on land. In the long term, the net carbon flux between forests and the atmosphere has been significantly impacted by changes in forest cover area and structure due to ecological disturbances and management activities. Current empirical approaches for estimating net ecosystem productivity (NEP) rarely consider forest age as a predictor, which represents vari…

  • Stomatal response to decreased relative humidity constrains the acceleration of terrestrial evapotranspiration

    Open Access•Mingzhong Xiao, Zhongbo Yu et al.•ARTICLE•Environmental Research Letters•2020

    Terrestrial evapotranspiration (ET) is thermodynamically expected to increase with increasing atmospheric temperature; however, the actual constraints on the intensification of ET remain uncertain due to a lack of direct observations. Based on the FLUXNET2015 Dataset, we found that relative humidity (RH) is a more important driver of ET than temperature. While actual ET decrease at reduced RH, potential ET increases, consistently with the complem…

  • Revealing how intra- and inter-annual variability of carbon uptake (GPP) affects wood cell biomass in an eastern white pine forest

    Open Access•Paulina F Puchi, Myroslava Khomik et al.•ARTICLE•Environmental Research Letters•2023

    Forests are major terrestrial carbon (C) sinks and play a crucial role in climate change mitigation. Despite extensive studies on forest C sequestration, the relationship between seasonal C uptake and its allocation to woody biomass is poorly understood. Here we used a novel dendro-anatomical approach to investigate the relationships between climate variability, C uptake, and woody biomass growth in an 80 year-old eastern white pine ( Pinus strob…

Environmental Science (8 works) · Atmospheric sciences (7 works) · Ecology (6 works) · Geography (6 works) · Plant Water Relations and Carbon Dynamics (6 works) · Climate change (5 works) · Climate variability and models (5 works) · Climatology (5 works) · Ecosystem (5 works) · Biology (4 works)

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