The western U.S., particularly the Southwest, has experienced a notable increase in record-breaking high temperatures over recent decades, with recurring drought and heatwaves.
These conditions have resulted in severe consequences for both human and nature systems, including dire water shortages, rampant wildfires, substantial agricultural losses, and increased human mortality. These regions, dominated by water-limited ecosystems, face exacerbated water stress due to more frequent and protracted droughts and heatwaves, which can profoundly impair ecosystem photosynthesis and carbon uptake, in turn affecting the global carbon cycle.
Investigating vegetation photosynthesis at various time scales provides valuable insights into vegetation growth, carbon uptake, and environmental interactions. Traditional polar-orbiting satellite observations have aided in monitoring gross primary production (GPP) at longer scales (e.g., monthly, annual), but they are limited in capturing diurnal variations. Fortunately, in recent years, emerging new-generation geostationary satellites with sub-daily sampling capability, provide unique opportunities to study diurnal variations of vegetation photosynthesis and their responses to environmental conditions over the course of day at large spatial scales.
Here we estimate hourly GPP across the Conterminous U.S. based on observations from Geostationary Operational Environmental Satellite-R (GOES-R), and then investigate how the diurnal cycle of photosynthesis responds to the severe late-summer heatwave of 2020. This study provides a comprehensive exploration of heatwave impacts on the diurnal dynamics of photosynthesis at a continental scale, revealing a widespread midday and afternoon depression of photosynthesis in dryland ecosystems during the heatwave. We examine the environmental regulation of diurnal photosynthesis dynamics across diverse ecosystems, and illustrate how current radiation-based methods for upscaling polar-orbiting satellite snapshots to daily means may under- or overestimate daily GPP.
Changes in environmental variables, gross primary production, and diurnal metrics during the heatwave from 14 to 19 August 2020 relative to 2018 and 2019 across the CONUS. (A) Standardized normalized anomalies of air temperature (Ta_ano, unitless) from MERRA-2 and diurnal centroid changes (units: hours) from 14 to 19 August 2020 relative to the multiyear average. (B) Different responses of diurnal metrics to the heatwave across vegetation types and along aridity gradients [smaller aridity index (AI) values indicate more arid conditions]. ENF, NENF (or non-ENF), SHR, SAV, GRA, and CRO represent evergreen needleleaf forest, other forests except for ENF, shrubland, savanna, grassland, and cropland, respectively. Box plots illustrate the distribution of diurnal change: The box represents the interquartile range (IQR), containing data from the 25th percentile (Q1) to the 75th percentile (Q3). The horizontal line inside the box indicates the median (50th percentile). The whiskers extend to the minimum and maximum values within 1.5 times the IQR from Q1 and Q3, respectively. The outliers beyond this range are plotted as individual red plus symbols. (C) Regional-mean hourly land surface temperature (LST), vapor pressure deficit (VPD), shortwave incoming radiation (SW), and gross primary production (GPP) for drylands and nondrylands in normal (black) and heatwave (red) years. C-heat, P-heat, and R-heat represent the diurnal centroid of GPP (CGPP), GPP peak hour (Hourpeak), and the ratio of afternoon GPP to morning GPP (RatioA/M) during the heatwave, while C-nor, P-nor, and R-nor represent these metrics in the normal years. The hours mentioned here correspond to local time.
□ Widespread midday and afternoon depression in ecosystem photosynthesis during the heatwave
We found a widespread midday and afternoon depression in ecosystem photosynthesis during the heatwave in the western United States. Diurnal centroid (CGPP) and peak hour of GPP shift toward earlier morning for the majority of the western regions, and the ratio of afternoon GPP to morning GPP also shows a marked decline. The shift in diurnal metrics positively correlates to the daily GPP change, implying that the morning shift in diurnal metrics generally results in a decrease in daily total GPP.
The diurnal metrics exhibit divergent responses to the heatwave across vegetation types and along aridity gradients. Overall, shrubland and grassland are more sensitive to the heatwave than the other vegetation types. The impact of the heatwave on the diurnal cycle of photosynthesis is predominantly observed in arid and semiarid regions with an aridity index (AI) below 0.6. We found that the largest GPP loss occurred at noon or during the afternoon for the majority of western regions, later than the GPP peak hour during the heatwave year, further substantiating the asymmetric influence of heatwaves on diurnal photosynthesis fluctuations.
□ Environmental controls on diurnal behavior of ecosystem photosynthesis
The regional-mean daily vapor pressure deficit (VPD) and land surface temperature (LST) show strong negative relationships with regional-mean CGPP, suggesting that the increase of heat and water stress contributes to an earlier coming of diurnal CGPP. The pixel-level relationships for different vegetation types show that shrubland has the strongest negative relationships and largest negative slopes between CGPP and VPD or LST among all the vegetation types, followed by evergreen needleleaf forest (ENF) and grassland.
□ Geostationary satellite-based method better estimates daily GPP and GPP loss during the heatwave
Our results clearly demonstrate that, using a snapshot from the earlier part of the morning (e.g., 8 a.m.) and solely considering radiation variations for daily upscaling lead to an overestimation of daily GPP across the majority of the United States. Conversely, using an afternoon observation for daily upscaling (e.g., 2 p.m.) results in an underestimation of daily GPP. The upscaling method relies only on radiation and does not account for changes induced by varying environmental stresses and light use efficiency throughout the day.
Biases stemming from the radiation-based upscaling method can also affect the calculation of GPP difference between normal and heatwave years. We further calculate the regional total daily GPP for drylands from 14 to 19 August for both years. Both daily GPP upscaling from all single hours and GPP capture the decline of dryland productivity during the heatwave. The estimated GPP loss for the entire region during the heatwave period based on GOES-R is approximately 0.4 Tg C per day, while GPP loss based on upscaling from different hours ranges from 0.25 to 0.6 Tg C per day.
The western U.S., particularly the Southwest, has experienced a notable increase in record-breaking high temperatures over recent decades, with recurring drought and heatwaves. These conditions have resulted in severe consequences for both human and nature systems, including dire water shortages, rampant wildfires, substantial agricultural losses, and increased human mortality. These regions, dominated by water-limited ecosystems, face exacerbated water stress due to more frequent and protracted droughts and heatwaves, which can profoundly impair ecosystem photosynthesis and carbon uptake, in turn affecting the global carbon cycle.
Investigating vegetation photosynthesis at various time scales provides valuable insights into vegetation growth, carbon uptake, and environmental interactions. Traditional polar-orbiting satellite observations have aided in monitoring gross primary production (GPP) at longer scales (e.g., monthly, annual), but they are limited in capturing diurnal variations. Fortunately, in recent years, emerging new-generation geostationary satellites with sub-daily sampling capability, provide unique opportunities to study diurnal variations of vegetation photosynthesis and their responses to environmental conditions over the course of day at large spatial scales.
Here we estimate hourly GPP across the Conterminous U.S. based on observations from Geostationary Operational Environmental Satellite-R (GOES-R), and then investigate how the diurnal cycle of photosynthesis responds to the severe late-summer heatwave of 2020. This study provides a comprehensive exploration of heatwave impacts on the diurnal dynamics of photosynthesis at a continental scale, revealing a widespread midday and afternoon depression of photosynthesis in dryland ecosystems during the heatwave. We examine the environmental regulation of diurnal photosynthesis dynamics across diverse ecosystems, and illustrate how current radiation-based methods for upscaling polar-orbiting satellite snapshots to daily means may under- or overestimate daily GPP.
□ Widespread midday and afternoon depression in ecosystem photosynthesis during the heatwave
We found a widespread midday and afternoon depression in ecosystem photosynthesis during the heatwave in the western United States. Diurnal centroid (CGPP) and peak hour of GPP shift toward earlier morning for the majority of the western regions, and the ratio of afternoon GPP to morning GPP also shows a marked decline. The shift in diurnal metrics positively correlates to the daily GPP change, implying that the morning shift in diurnal metrics generally results in a decrease in daily total GPP.
The diurnal metrics exhibit divergent responses to the heatwave across vegetation types and along aridity gradients. Overall, shrubland and grassland are more sensitive to the heatwave than the other vegetation types. The impact of the heatwave on the diurnal cycle of photosynthesis is predominantly observed in arid and semiarid regions with an aridity index (AI) below 0.6. We found that the largest GPP loss occurred at noon or during the afternoon for the majority of western regions, later than the GPP peak hour during the heatwave year, further substantiating the asymmetric influence of heatwaves on diurnal photosynthesis fluctuations.
□ Environmental controls on diurnal behavior of ecosystem photosynthesis
The regional-mean daily vapor pressure deficit (VPD) and land surface temperature (LST) show strong negative relationships with regional-mean CGPP, suggesting that the increase of heat and water stress contributes to an earlier coming of diurnal CGPP. The pixel-level relationships for different vegetation types show that shrubland has the strongest negative relationships and largest negative slopes between CGPP and VPD or LST among all the vegetation types, followed by evergreen needleleaf forest (ENF) and grassland.
□ Geostationary satellite-based method better estimates daily GPP and GPP loss during the heatwave
Our results clearly demonstrate that, using a snapshot from the earlier part of the morning (e.g., 8 a.m.) and solely considering radiation variations for daily upscaling lead to an overestimation of daily GPP across the majority of the United States. Conversely, using an afternoon observation for daily upscaling (e.g., 2 p.m.) results in an underestimation of daily GPP. The upscaling method relies only on radiation and does not account for changes induced by varying environmental stresses and light use efficiency throughout the day.
Biases stemming from the radiation-based upscaling method can also affect the calculation of GPP difference between normal and heatwave years. We further calculate the regional total daily GPP for drylands from 14 to 19 August for both years. Both daily GPP upscaling from all single hours and GPP capture the decline of dryland productivity during the heatwave. The estimated GPP loss for the entire region during the heatwave period based on GOES-R is approximately 0.4 Tg C per day, while GPP loss based on upscaling from different hours ranges from 0.25 to 0.6 Tg C per day.
New-generation geostationary satellite reveals widespread midday depression in dryland photosynthesis during 2020 western U.S. heatwave, Science (open access)
