Zobrazeno 1 - 10
of 25
pro vyhledávání: '"D. Jenerette"'
Publikováno v:
Biogeosciences, Vol 14, Iss 9, Pp 2513-2525 (2017)
The frequency of dry-season droughts and wet-season storms has been predicted to increase in subtropical areas in the coming decades. Since subtropical forest soils are significant sources of N2O and NO3−, it is important to understand the features
Externí odkaz:
https://doaj.org/article/d07caab15ada477e878a64778c2e1e80
Publikováno v:
Biogeosciences, Vol 13, Iss 2, Pp 425-439 (2016)
The precipitation legacy effect, defined as the impact of historical precipitation (PPT) on extant ecosystem dynamics, has been recognized as an important driver in shaping the temporal variability of dryland aboveground net primary production (ANPP)
Externí odkaz:
https://doaj.org/article/3c95569e4cd34837bd33aa058a087320
Publikováno v:
Environmental Research Letters, Vol 12, Iss 8, p 084007 (2017)
Urban vegetation provides many highly valued ecosystem services but also requires extensive urban water resources. Increasingly, cities are experiencing water limitations and managing outdoor urban water use is an important concern. Quantifying the w
Externí odkaz:
https://doaj.org/article/cab072795b5047bfaafdd2e2bca68e69
Autor:
D. Jenerette, Jon K Botthoff, James O. Sickman, Peter M. Homyak, Alex Krichels, Stephanie Piper, Aral C. Greene, Emma L. Aronson, Jun Wang, Hannah Shulman
Nitrogen deposition into arid ecosystems is increasingly shaping biogeochemical dynamics worldwide. We propose a framework to investigate the role of pulsed soil N emission as a mechanism that relays the influences of atmospheric anthropogenic N depo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f32350ffb9b2961348327ed1de76f1f5
https://doi.org/10.5194/egusphere-egu2020-21311
https://doi.org/10.5194/egusphere-egu2020-21311
Publikováno v:
Environmental Research Letters, Vol 10, Iss 3, p 034008 (2015)
Carbon (C) and nitrogen (N) interactions contribute to uncertainty in current biogeochemical models that aim to estimate greenhouse gas (GHG, including CO _2 and N _2 O) emissions from soil to atmosphere. In this study, we quantified CO _2 and N _2 O
Externí odkaz:
https://doaj.org/article/18fe00fa39224af8b55a074e6d7206d5
Autor:
Joseph Verfaillie, Sara H. Knox, Patricia Y. Oikawa, Elke Eichelmann, Dennis D. Baldocchi, Iryna Dronova, G. D. Jenerette, Cristina Poindexter, Cove Sturtevant
Publikováno v:
Journal of Geophysical Research: Biogeosciences. 122:145-167
Wetlands and flooded peatlands can sequester large amounts of carbon (C) and have high greenhouse gas mitigation potential. There is growing interest in financing wetland restoration using C markets; however, this requires careful accounting of both
Publikováno v:
Biogeosciences, Vol 13, Iss 2, Pp 425-439 (2016)
The precipitation legacy effect, defined as the impact of historical precipitation (PPT) on extant ecosystem dynamics, has been recognized as an important driver in shaping the temporal variability of dryland aboveground primary production (ANPP) and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::366dde4c8c5c2a97cfd8ff141c3a5c66
https://www.biogeosciences.net/13/425/2016/
https://www.biogeosciences.net/13/425/2016/
Publikováno v:
Journal of Arid Land. 7:814-819
Variations in soil organic matter accumulation across an elevation can be used to explain the control of substrate supply and variability on soil metabolic activity. We investigated geographic changes in soil organic matter and metabolic rates along
Publikováno v:
Soil Biology and Biochemistry. 88:158-164
The response of soil CO2 fluxes (Rsoil) to interactions between carbon (C) and nitrogen (N) availability or C and temperature conditions is not well understood, but may increasingly affect future C storage under the combined anthropogenic impacts of
Autor:
Matei Georgescu, Winston T. L. Chow, S. R. Shaffer, Peter Hyde, Alex Mahalov, Mohamed Moustaoui, Benjamin L. Ruddell, G. D. Jenerette
Publikováno v:
Journal of Applied Meteorology and Climatology. 54:322-338
Physical mechanisms of incongruency between observations and Weather Research and Forecasting (WRF) Model predictions are examined. Limitations of evaluation are constrained by (i) parameterizations of model physics, (ii) parameterizations of input d