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I Colin Prentice

Showing results (21-30 of 68) with videos related to

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The New Phytologist|April 2, 2026
An eco-evolutionary optimality model explains the acclimated temperature response of photosynthesisWenyao Gan, Nabil Alizadeh, Martin Best, et al.
The New Phytologist|November 19, 2016
Photosynthetic responses to altitude: an explanation based on optimality principlesHan Wang, I Colin Prentice, Tyler W Davis, et al.
The New Phytologist|April 1, 2018
Quantifying soil moisture impacts on light use efficiency across biomesBenjamin D Stocker, Jakob Zscheischler, Trevor F Keenan, et al.
Climate Dynamics|December 22, 2025
Influence of global climate modes on wildfire occurrence in the contiguous United States under recent and future climatesTheodore R Keeping, Theodore G Shepherd, I Colin Prentice, et al.
The New Phytologist|October 2, 2018
Quantifying leaf-trait covariation and its controls across climates and biomesYanzheng Yang, Han Wang, Sandy P Harrison, et al.
Scientific Reports|February 25, 2017
Changes in biomass allocation buffer low CO<sub>2</sub> effects on tree growth during the last glaciationGuangqi Li, Laci M Gerhart, Sandy P Harrison, et al.
Ecological Applications : a Publication of the Ecological Society of America|August 30, 2006
The importance of age-related decline in forest NPP for modeling regional carbon balancesSönke Zaehle, Stephen Sitch, I Colin Prentice, et al.
Plos One|December 21, 2013
Relationships between human population density and burned area at continental and global scalesIoannis Bistinas, Duarte Oom, Ana C L Sá, et al.
Nature Communications|July 15, 2017
Corrigendum: Recent pause in the growth rate of atmospheric CO<sub>2</sub> due to enhanced terrestrial carbon uptakeTrevor F Keenan, I Colin Prentice, Josep G Canadell, et al.
Nature Communications|November 9, 2016
Recent pause in the growth rate of atmospheric CO<sub>2</sub> due to enhanced terrestrial carbon uptakeTrevor F Keenan, I Colin Prentice, Josep G Canadell, et al.
Pageof 7

Showing results (21-30 of 68) with videos related to

Sort By:
Pageof 7
The New Phytologist|April 2, 2026
An eco-evolutionary optimality model explains the acclimated temperature response of photosynthesisWenyao Gan, Nabil Alizadeh, Martin Best, et al.
The New Phytologist|November 19, 2016
Photosynthetic responses to altitude: an explanation based on optimality principlesHan Wang, I Colin Prentice, Tyler W Davis, et al.
The New Phytologist|April 1, 2018
Quantifying soil moisture impacts on light use efficiency across biomesBenjamin D Stocker, Jakob Zscheischler, Trevor F Keenan, et al.
Climate Dynamics|December 22, 2025
Influence of global climate modes on wildfire occurrence in the contiguous United States under recent and future climatesTheodore R Keeping, Theodore G Shepherd, I Colin Prentice, et al.
The New Phytologist|October 2, 2018
Quantifying leaf-trait covariation and its controls across climates and biomesYanzheng Yang, Han Wang, Sandy P Harrison, et al.
Scientific Reports|February 25, 2017
Changes in biomass allocation buffer low CO<sub>2</sub> effects on tree growth during the last glaciationGuangqi Li, Laci M Gerhart, Sandy P Harrison, et al.
Ecological Applications : a Publication of the Ecological Society of America|August 30, 2006
The importance of age-related decline in forest NPP for modeling regional carbon balancesSönke Zaehle, Stephen Sitch, I Colin Prentice, et al.
Plos One|December 21, 2013
Relationships between human population density and burned area at continental and global scalesIoannis Bistinas, Duarte Oom, Ana C L Sá, et al.
Nature Communications|July 15, 2017
Corrigendum: Recent pause in the growth rate of atmospheric CO<sub>2</sub> due to enhanced terrestrial carbon uptakeTrevor F Keenan, I Colin Prentice, Josep G Canadell, et al.
Nature Communications|November 9, 2016
Recent pause in the growth rate of atmospheric CO<sub>2</sub> due to enhanced terrestrial carbon uptakeTrevor F Keenan, I Colin Prentice, Josep G Canadell, et al.
Pageof 7