Geology topics

Jack A. Morgan

Publications and source records attributed to Jack A. Morgan.

3 recordsLinked to original sources

USGS2017

Productivity and CO 2 exchange of Great Plains ecoregions. I. Shortgrass steppe: Flux tower estimates

The shortgrass steppe (SGS) occupies the southwestern part of the Great Plains. Half of the land is cultivated, but significant areas remain under natural vegetation. Despite previous studies of the SGS carbon cycle, not all aspects have been completely addressed, including gross productivity, ecosystem respiration, and ecophysiological parameters. Our analysis of 1998 − 2007 flux tower measurements at five Bowen ratio–energy balance (BREB) and three eddy covariance (EC) sites characterized seasonal and interannual variability of gross photosynthesis and ecosystem respiration. Identification of the nonrectangular hyperbolic equation for the diurnal CO 2 exchange, with vapor pressure deficit (VPD) limitation and exponential temperature response, quantified quantum yield α , photosynthetic capacity A max , and respiration rate r d with variation ranges (19 \< α \ < 51 mmol mol − 1 , 0.48 \< A max \ < 2.1 mg CO 2 m − 2 s − 1 , 0.15 \< r d \ < 0.49 mg CO 2 m − 2 s − 1 ). Gross photosynthesis varied from 1 100 to 2 700 g CO 2 m − 2 yr − 1 , respiration from 900 to 3,000 g CO 2 m − 2 yr − 1 , and net ecosystem production from − 900 to + 700 g CO 2 m − 2 yr − 1 , indicating that SGS may switch from a sink to a source depending on weather. Comparison of the 2004 − 2006 measurements at two BREB and two parallel EC flux towers located at comparable SGS sites showed moderately higher photosynthesis, lower respiration, and higher net production at the BREB than EC sites. However, the difference was not related only to methodologies, as the normalized difference vegetation index at the BREB sites was higher than at the EC sites. Overall magnitudes and seasonal patterns at the BREB and the EC sites during the 3-yr period were similar, with trajectories within the ± 1.5 standard deviation around the mean of the four sites and mostly reflecting the effects of meteorology.

Colorado, Wyoming↗

USGS2012

Elevated CO2 does not offset greater water stress predicted under climate change for native and exotic riparian plants

In semiarid western North American riparian ecosystems, increased drought and lower streamflows under climate change may reduce plant growth and recruitment, and favor drought‐tolerant exotic species over mesic native species. We tested whether elevated atmospheric CO 2 might ameliorate these effects by improving plant water‐use efficiency. We examined the effects of CO 2 and water availability on seedlings of two native ( Populus deltoides spp. monilifera , Salix exigua ) and three exotic ( Elaeagnus angustifolia , Tamarix spp., Ulmus pumila ) western North American riparian species in a CO 2 ‐controlled glasshouse, using 1‐m‐deep pots with different water‐table decline rates. Low water availability reduced seedling biomass by 70–97%, and hindered the native species more than the exotics. Elevated CO 2 increased biomass by 15%, with similar effects on natives and exotics. Elevated CO 2 increased intrinsic water‐use efficiency (Δ 13 C leaf ), but did not increase biomass more in drier treatments than wetter treatments. The moderate positive effects of elevated CO 2 on riparian seedlings are unlikely to counteract the large negative effects of increased aridity projected under climate change. Our results suggest that increased aridity will reduce riparian seedling growth despite elevated CO 2 , and will reduce growth more for native Salix and Populus than for drought‐tolerant exotic species.

New Phytologist↗

USGS2005

Integration of CO2 flux and remotely-sensed data for primary production and ecosystem respiration analyses in the Northern Great Plains: potential for quantitative spatial extrapolation

Aim&ensp; Extrapolation of tower CO 2 fluxes will be greatly facilitated if robust relationships between flux components and remotely sensed factors are established. Long-term measurements at five Northern Great Plains locations were used to obtain relationships between CO 2 fluxes and photosynthetically active radiation ( Q ), other on-site factors, and Normalized Difference Vegetation Index ( NDVI ) from the SPOT VEGETATION data set. Location&ensp; CO 2 flux data from the following stations and years were analysed: Lethbridge, Alberta 1998–2001; Fort Peck, MT 2000, 2002; Miles City, MT 2000–01; Mandan, ND 1999–2001; and Cheyenne, WY 1997–98. Results&ensp; Analyses based on light-response functions allowed partitioning net CO 2 flux ( F ) into gross primary productivity ( P g ) and ecosystem respiration ( R e ). Weekly averages of daytime respiration, γ day , estimated from light responses were closely correlated with weekly averages of measured night-time respiration, γ night ( R 2 0.64 to 0.95). Daytime respiration tended to be higher than night-time respiration, and regressions of γ day on γ night for all sites were different from 1 : 1 relationships. Over 13 site-years, gross primary production varied from 459 to 2491 g CO 2 m −2 year −1 , ecosystem respiration from 996 to 1881 g CO 2 m −2 year −1 , and net ecosystem exchange from −537 (source) to +610 g CO 2 m −2 year −1 (sink). Maximum daily ecological light-use efficiencies, ɛ d , max = P g /Q , were in the range 0.014 to 0.032 mol CO 2 (mol incident quanta) −1 . Main conclusions&ensp; Ten-day average P g was significantly more highly correlated with NDVI than 10-day average daytime flux, P d ( R 2 = 0.46 to 0.77 for P g -NDVI and 0.05 to 0.58 for P d -NDVI relationships). Ten-day average R e was also positively correlated with NDVI , with R 2 values from 0.57 to 0.77. Patterns of the relationships of P g and R e with NDVI and other factors indicate possibilities for establishing multivariate functions allowing scaling-up local fluxes to larger areas using GIS data, temporal NDVI, and other factors.

Global Ecology and Biogeography↗