Improvement of modeling plant responses to low soil moisture in JULESvn4.9 and evaluation against flux tower measurements

Abstract. Drought is predicted to increase in the future due to climate change, bringing with it myriad impacts on ecosystems. Plants respond to drier soils by reducing stomatal conductance in order to conserve water and avoid hydraulic damage. Despite the importance of plant drought responses for t...

Descripción completa

Detalles Bibliográficos
Autores principales: Harper, Anna B., Williams, Karina E., McGuire, Patrick C., Duran Rojas, Maria Carolina, Hemming, Debbie, Verhoef, Anne, Huntingford, Chris, Rowland, Lucy, Marthews, Toby, Breder Eller, Cleiton, Mathison, Camilla, Nobrega, Rodolfo L.B., Gedney, Nicola, Vidale, Pier Luigi, Otu-Larbi, Fred, Pandey, Divya, Garrigues, Sebastien, Wright, Azin, Slevin, Darren, Kauwe, Martin G. de, Blyth, Eleanor, Ardö, Jonas, Black, Andrew, Bonal, Damien, Buchmann, Nina, Burban, Benoit, Fuchs, Kathrin, Grandcourt, Agnès de, Mammarella, Ivan, Merbold, Lutz, Montagnani, Leonardo, Nouvellon, Yann, Restrepo Coupe, Natalia, Wohlfahrt, Georg
Formato: Journal Article
Lenguaje:Inglés
Publicado: Copernicus GmbH 2021
Materias:
Acceso en línea:https://hdl.handle.net/10568/129375
_version_ 1855527044478140416
author Harper, Anna B.
Williams, Karina E.
McGuire, Patrick C.
Duran Rojas, Maria Carolina
Hemming, Debbie
Verhoef, Anne
Huntingford, Chris
Rowland, Lucy
Marthews, Toby
Breder Eller, Cleiton
Mathison, Camilla
Nobrega, Rodolfo L.B.
Gedney, Nicola
Vidale, Pier Luigi
Otu-Larbi, Fred
Pandey, Divya
Garrigues, Sebastien
Wright, Azin
Slevin, Darren
Kauwe, Martin G. de
Blyth, Eleanor
Ardö, Jonas
Black, Andrew
Bonal, Damien
Buchmann, Nina
Burban, Benoit
Fuchs, Kathrin
Grandcourt, Agnès de
Mammarella, Ivan
Merbold, Lutz
Montagnani, Leonardo
Nouvellon, Yann
Restrepo Coupe, Natalia
Wohlfahrt, Georg
author_browse Ardö, Jonas
Black, Andrew
Blyth, Eleanor
Bonal, Damien
Breder Eller, Cleiton
Buchmann, Nina
Burban, Benoit
Duran Rojas, Maria Carolina
Fuchs, Kathrin
Garrigues, Sebastien
Gedney, Nicola
Grandcourt, Agnès de
Harper, Anna B.
Hemming, Debbie
Huntingford, Chris
Kauwe, Martin G. de
Mammarella, Ivan
Marthews, Toby
Mathison, Camilla
McGuire, Patrick C.
Merbold, Lutz
Montagnani, Leonardo
Nobrega, Rodolfo L.B.
Nouvellon, Yann
Otu-Larbi, Fred
Pandey, Divya
Restrepo Coupe, Natalia
Rowland, Lucy
Slevin, Darren
Verhoef, Anne
Vidale, Pier Luigi
Williams, Karina E.
Wohlfahrt, Georg
Wright, Azin
author_facet Harper, Anna B.
Williams, Karina E.
McGuire, Patrick C.
Duran Rojas, Maria Carolina
Hemming, Debbie
Verhoef, Anne
Huntingford, Chris
Rowland, Lucy
Marthews, Toby
Breder Eller, Cleiton
Mathison, Camilla
Nobrega, Rodolfo L.B.
Gedney, Nicola
Vidale, Pier Luigi
Otu-Larbi, Fred
Pandey, Divya
Garrigues, Sebastien
Wright, Azin
Slevin, Darren
Kauwe, Martin G. de
Blyth, Eleanor
Ardö, Jonas
Black, Andrew
Bonal, Damien
Buchmann, Nina
Burban, Benoit
Fuchs, Kathrin
Grandcourt, Agnès de
Mammarella, Ivan
Merbold, Lutz
Montagnani, Leonardo
Nouvellon, Yann
Restrepo Coupe, Natalia
Wohlfahrt, Georg
author_sort Harper, Anna B.
collection Repository of Agricultural Research Outputs (CGSpace)
description Abstract. Drought is predicted to increase in the future due to climate change, bringing with it myriad impacts on ecosystems. Plants respond to drier soils by reducing stomatal conductance in order to conserve water and avoid hydraulic damage. Despite the importance of plant drought responses for the global carbon cycle and local and regional climate feedbacks, land surface models are unable to capture observed plant responses to soil moisture stress. We assessed the impact of soil moisture stress on simulated gross primary productivity (GPP) and latent energy flux (LE) in the Joint UK Land Environment Simulator (JULES) vn4.9 on seasonal and annual timescales and evaluated 10 different representations of soil moisture stress in the model. For the default configuration, GPP was more realistic in temperate biome sites than in the tropics or high-latitude (cold-region) sites, while LE was best simulated in temperate and high-latitude (cold) sites. Errors that were not due to soil moisture stress, possibly linked to phenology, contributed to model biases for GPP in tropical savanna and deciduous forest sites. We found that three alternative approaches to calculating soil moisture stress produced more realistic results than the default parameterization for most biomes and climates. All of these involved increasing the number of soil layers from 4 to 14 and the soil depth from 3.0 to 10.8 m. In addition, we found improvements when soil matric potential replaced volumetric water content in the stress equation (the “soil14_psi” experiments), when the critical threshold value for inducing soil moisture stress was reduced (“soil14_p0”), and when plants were able to access soil moisture in deeper soil layers (“soil14_dr*2”). For LE, the biases were highest in the default configuration in temperate mixed forests, with overestimation occurring during most of the year. At these sites, reducing soil moisture stress (with the new parameterizations mentioned above) increased LE and increased model biases but improved the simulated seasonal cycle and brought the monthly variance closer to the measured variance of LE. Further evaluation of the reason for the high bias in LE at many of the sites would enable improvements in both carbon and energy fluxes with new parameterizations for soil moisture stress. Increasing the soil depth and plant access to deep soil moisture improved many aspects of the simulations, and we recommend these settings in future work using JULES or as a general way to improve land surface carbon and water fluxes in other models. In addition, using soil matric potential presents the opportunity to include plant functional type-specific parameters to further improve modeled fluxes.
format Journal Article
id CGSpace129375
institution CGIAR Consortium
language Inglés
publishDate 2021
publishDateRange 2021
publishDateSort 2021
publisher Copernicus GmbH
publisherStr Copernicus GmbH
record_format dspace
spelling CGSpace1293752025-12-08T10:11:39Z Improvement of modeling plant responses to low soil moisture in JULESvn4.9 and evaluation against flux tower measurements Harper, Anna B. Williams, Karina E. McGuire, Patrick C. Duran Rojas, Maria Carolina Hemming, Debbie Verhoef, Anne Huntingford, Chris Rowland, Lucy Marthews, Toby Breder Eller, Cleiton Mathison, Camilla Nobrega, Rodolfo L.B. Gedney, Nicola Vidale, Pier Luigi Otu-Larbi, Fred Pandey, Divya Garrigues, Sebastien Wright, Azin Slevin, Darren Kauwe, Martin G. de Blyth, Eleanor Ardö, Jonas Black, Andrew Bonal, Damien Buchmann, Nina Burban, Benoit Fuchs, Kathrin Grandcourt, Agnès de Mammarella, Ivan Merbold, Lutz Montagnani, Leonardo Nouvellon, Yann Restrepo Coupe, Natalia Wohlfahrt, Georg evaluation soil soil moisture improvement plant Abstract. Drought is predicted to increase in the future due to climate change, bringing with it myriad impacts on ecosystems. Plants respond to drier soils by reducing stomatal conductance in order to conserve water and avoid hydraulic damage. Despite the importance of plant drought responses for the global carbon cycle and local and regional climate feedbacks, land surface models are unable to capture observed plant responses to soil moisture stress. We assessed the impact of soil moisture stress on simulated gross primary productivity (GPP) and latent energy flux (LE) in the Joint UK Land Environment Simulator (JULES) vn4.9 on seasonal and annual timescales and evaluated 10 different representations of soil moisture stress in the model. For the default configuration, GPP was more realistic in temperate biome sites than in the tropics or high-latitude (cold-region) sites, while LE was best simulated in temperate and high-latitude (cold) sites. Errors that were not due to soil moisture stress, possibly linked to phenology, contributed to model biases for GPP in tropical savanna and deciduous forest sites. We found that three alternative approaches to calculating soil moisture stress produced more realistic results than the default parameterization for most biomes and climates. All of these involved increasing the number of soil layers from 4 to 14 and the soil depth from 3.0 to 10.8 m. In addition, we found improvements when soil matric potential replaced volumetric water content in the stress equation (the “soil14_psi” experiments), when the critical threshold value for inducing soil moisture stress was reduced (“soil14_p0”), and when plants were able to access soil moisture in deeper soil layers (“soil14_dr*2”). For LE, the biases were highest in the default configuration in temperate mixed forests, with overestimation occurring during most of the year. At these sites, reducing soil moisture stress (with the new parameterizations mentioned above) increased LE and increased model biases but improved the simulated seasonal cycle and brought the monthly variance closer to the measured variance of LE. Further evaluation of the reason for the high bias in LE at many of the sites would enable improvements in both carbon and energy fluxes with new parameterizations for soil moisture stress. Increasing the soil depth and plant access to deep soil moisture improved many aspects of the simulations, and we recommend these settings in future work using JULES or as a general way to improve land surface carbon and water fluxes in other models. In addition, using soil matric potential presents the opportunity to include plant functional type-specific parameters to further improve modeled fluxes. 2021-06-03 2023-03-10T14:33:59Z 2023-03-10T14:33:59Z Journal Article https://hdl.handle.net/10568/129375 en Open Access Copernicus GmbH Harper, Anna B.; Williams, Karina E.; McGuire, Patrick C.; Duran Rojas, Maria Carolina; Hemming, Debbie; Verhoef, Anne; Huntingford, Chris; Rowland, Lucy; Marthews, Toby; Breder Eller, Cleiton; Mathison, Camilla; Nobrega, Rodolfo L.B.; Gedney, Nicola; Vidale, Pier Luigi; Otu-Larbi, Fred; Pandey, Divya; Garrigues, Sebastien; Wright, Azin; Slevin, Darren; Kauwe, Martin G. de; Blyth, Eleanor; Ardö, Jonas; Black, Andrew; Bonal, Damien; Buchmann, Nina; Burban, Benoit; Fuchs, Kathrin; Grandcourt, Agnès de; Mammarella, Ivan; Merbold, Lutz; Montagnani, Leonardo; Nouvellon, Yann; Restrepo-Coupe, Natalia; Wohlfahrt, Georg. 2021. Improvement of modeling plant responses to low soil moisture in JULESvn4.9 and evaluation against flux tower measurements. Geoscientific Model Development 14: 3269-3294
spellingShingle evaluation
soil
soil moisture
improvement
plant
Harper, Anna B.
Williams, Karina E.
McGuire, Patrick C.
Duran Rojas, Maria Carolina
Hemming, Debbie
Verhoef, Anne
Huntingford, Chris
Rowland, Lucy
Marthews, Toby
Breder Eller, Cleiton
Mathison, Camilla
Nobrega, Rodolfo L.B.
Gedney, Nicola
Vidale, Pier Luigi
Otu-Larbi, Fred
Pandey, Divya
Garrigues, Sebastien
Wright, Azin
Slevin, Darren
Kauwe, Martin G. de
Blyth, Eleanor
Ardö, Jonas
Black, Andrew
Bonal, Damien
Buchmann, Nina
Burban, Benoit
Fuchs, Kathrin
Grandcourt, Agnès de
Mammarella, Ivan
Merbold, Lutz
Montagnani, Leonardo
Nouvellon, Yann
Restrepo Coupe, Natalia
Wohlfahrt, Georg
Improvement of modeling plant responses to low soil moisture in JULESvn4.9 and evaluation against flux tower measurements
title Improvement of modeling plant responses to low soil moisture in JULESvn4.9 and evaluation against flux tower measurements
title_full Improvement of modeling plant responses to low soil moisture in JULESvn4.9 and evaluation against flux tower measurements
title_fullStr Improvement of modeling plant responses to low soil moisture in JULESvn4.9 and evaluation against flux tower measurements
title_full_unstemmed Improvement of modeling plant responses to low soil moisture in JULESvn4.9 and evaluation against flux tower measurements
title_short Improvement of modeling plant responses to low soil moisture in JULESvn4.9 and evaluation against flux tower measurements
title_sort improvement of modeling plant responses to low soil moisture in julesvn4 9 and evaluation against flux tower measurements
topic evaluation
soil
soil moisture
improvement
plant
url https://hdl.handle.net/10568/129375
work_keys_str_mv AT harperannab improvementofmodelingplantresponsestolowsoilmoistureinjulesvn49andevaluationagainstfluxtowermeasurements
AT williamskarinae improvementofmodelingplantresponsestolowsoilmoistureinjulesvn49andevaluationagainstfluxtowermeasurements
AT mcguirepatrickc improvementofmodelingplantresponsestolowsoilmoistureinjulesvn49andevaluationagainstfluxtowermeasurements
AT duranrojasmariacarolina improvementofmodelingplantresponsestolowsoilmoistureinjulesvn49andevaluationagainstfluxtowermeasurements
AT hemmingdebbie improvementofmodelingplantresponsestolowsoilmoistureinjulesvn49andevaluationagainstfluxtowermeasurements
AT verhoefanne improvementofmodelingplantresponsestolowsoilmoistureinjulesvn49andevaluationagainstfluxtowermeasurements
AT huntingfordchris improvementofmodelingplantresponsestolowsoilmoistureinjulesvn49andevaluationagainstfluxtowermeasurements
AT rowlandlucy improvementofmodelingplantresponsestolowsoilmoistureinjulesvn49andevaluationagainstfluxtowermeasurements
AT marthewstoby improvementofmodelingplantresponsestolowsoilmoistureinjulesvn49andevaluationagainstfluxtowermeasurements
AT brederellercleiton improvementofmodelingplantresponsestolowsoilmoistureinjulesvn49andevaluationagainstfluxtowermeasurements
AT mathisoncamilla improvementofmodelingplantresponsestolowsoilmoistureinjulesvn49andevaluationagainstfluxtowermeasurements
AT nobregarodolfolb improvementofmodelingplantresponsestolowsoilmoistureinjulesvn49andevaluationagainstfluxtowermeasurements
AT gedneynicola improvementofmodelingplantresponsestolowsoilmoistureinjulesvn49andevaluationagainstfluxtowermeasurements
AT vidalepierluigi improvementofmodelingplantresponsestolowsoilmoistureinjulesvn49andevaluationagainstfluxtowermeasurements
AT otularbifred improvementofmodelingplantresponsestolowsoilmoistureinjulesvn49andevaluationagainstfluxtowermeasurements
AT pandeydivya improvementofmodelingplantresponsestolowsoilmoistureinjulesvn49andevaluationagainstfluxtowermeasurements
AT garriguessebastien improvementofmodelingplantresponsestolowsoilmoistureinjulesvn49andevaluationagainstfluxtowermeasurements
AT wrightazin improvementofmodelingplantresponsestolowsoilmoistureinjulesvn49andevaluationagainstfluxtowermeasurements
AT slevindarren improvementofmodelingplantresponsestolowsoilmoistureinjulesvn49andevaluationagainstfluxtowermeasurements
AT kauwemartingde improvementofmodelingplantresponsestolowsoilmoistureinjulesvn49andevaluationagainstfluxtowermeasurements
AT blytheleanor improvementofmodelingplantresponsestolowsoilmoistureinjulesvn49andevaluationagainstfluxtowermeasurements
AT ardojonas improvementofmodelingplantresponsestolowsoilmoistureinjulesvn49andevaluationagainstfluxtowermeasurements
AT blackandrew improvementofmodelingplantresponsestolowsoilmoistureinjulesvn49andevaluationagainstfluxtowermeasurements
AT bonaldamien improvementofmodelingplantresponsestolowsoilmoistureinjulesvn49andevaluationagainstfluxtowermeasurements
AT buchmannnina improvementofmodelingplantresponsestolowsoilmoistureinjulesvn49andevaluationagainstfluxtowermeasurements
AT burbanbenoit improvementofmodelingplantresponsestolowsoilmoistureinjulesvn49andevaluationagainstfluxtowermeasurements
AT fuchskathrin improvementofmodelingplantresponsestolowsoilmoistureinjulesvn49andevaluationagainstfluxtowermeasurements
AT grandcourtagnesde improvementofmodelingplantresponsestolowsoilmoistureinjulesvn49andevaluationagainstfluxtowermeasurements
AT mammarellaivan improvementofmodelingplantresponsestolowsoilmoistureinjulesvn49andevaluationagainstfluxtowermeasurements
AT merboldlutz improvementofmodelingplantresponsestolowsoilmoistureinjulesvn49andevaluationagainstfluxtowermeasurements
AT montagnanileonardo improvementofmodelingplantresponsestolowsoilmoistureinjulesvn49andevaluationagainstfluxtowermeasurements
AT nouvellonyann improvementofmodelingplantresponsestolowsoilmoistureinjulesvn49andevaluationagainstfluxtowermeasurements
AT restrepocoupenatalia improvementofmodelingplantresponsestolowsoilmoistureinjulesvn49andevaluationagainstfluxtowermeasurements
AT wohlfahrtgeorg improvementofmodelingplantresponsestolowsoilmoistureinjulesvn49andevaluationagainstfluxtowermeasurements