TY - JOUR
T1 - Designing a network of critical zone observatories to explore the living skin of the terrestrial Earth
AU - Brantley, Susan L.
AU - McDowell, William H.
AU - Dietrich, William E.
AU - White, Timothy S.
AU - Kumar, Praveen
AU - Anderson, Suzanne P.
AU - Chorover, Jon
AU - Ann Lohse, Kathleen
AU - Bales, Roger C.
AU - Richter, Daniel D.
AU - Grant, Gordon
AU - Gaillardet, Jerome
N1 - Funding Information:
Abstract. The critical zone (CZ), the dynamic living skin of the Earth, extends from the top of the vegetative canopy through the soil and down to fresh bedrock and the bottom of the groundwater. All humans live in and depend on the CZ. This zone has three co-evolving surfaces: the top of the vegetative canopy, the ground surface, and a deep subsurface below which Earth’s materials are unweathered. The network of nine CZ observatories supported by the US National Science Foundation has made advances in three broad areas of CZ research relating to the co-evolving surfaces. First, monitoring has revealed how natural and anthropogenic inputs at the vegetation canopy and ground surface cause subsurface responses in water, regolith structure, minerals, and biotic activity to considerable depths. This response, in turn, impacts aboveground biota and climate. Second, drilling and geophysical imaging now reveal how the deep subsurface of the CZ varies across landscapes, which in turn influences aboveground ecosystems. Third, several new mechanistic models now provide quantitative predictions of the spatial structure of the subsurface of the CZ.
Funding Information:
We acknowledge the help of Sarah Sharkey (funded by the CZO Science Across Virtual Institutes Project), Jennifer Williams, Tracy Bernier, and Debra Lambert, and funding from NSF grants EAR 13-31726 to Susan L. Brantley, EAR 13-31906 to Praveen Kumar, EAR 13-31872 to Kathleen A. Lohse, EAR 13-31846 to Daniel deB. Richter, EAR 13-31408 to Jon Chorover, EAR13-31828 to Suzanne Anderson, EAR 14-45246 to Timothy S. White, EAR 13-31841 to William H. McDowell, and EAR13-31940 to William E. Dietrich. The paper benefitted from reviews by Jon Tunnicliffe and the anonymous reviewer, and comments from Kevin Bishop, Paul Schroeder, and Elisabeth Bui, and editorial handling by Jens Turowski.
Funding Information:
For example, individual grants (example (i) from above) can test sharply focused hypotheses that may lead to important discoveries about individual entities or processes. This kind of research, typically supported by a core grant from within a specific discipline (e.g., hydrology) sustains both the discipline and advances CZ science. The last decades of research have clearly shown that some advances come from single-investigator research.
PY - 2017/12/18
Y1 - 2017/12/18
N2 - The critical zone (CZ), the dynamic living skin of the Earth, extends from the top of the vegetative canopy through the soil and down to fresh bedrock and the bottom of the groundwater. All humans live in and depend on the CZ. This zone has three co-evolving surfaces: the top of the vegetative canopy, the ground surface, and a deep subsurface below which Earth's materials are unweathered. The network of nine CZ observatories supported by the US National Science Foundation has made advances in three broad areas of CZ research relating to the co-evolving surfaces. First, monitoring has revealed how natural and anthropogenic inputs at the vegetation canopy and ground surface cause subsurface responses in water, regolith structure, minerals, and biotic activity to considerable depths. This response, in turn, impacts aboveground biota and climate. Second, drilling and geophysical imaging now reveal how the deep subsurface of the CZ varies across landscapes, which in turn influences aboveground ecosystems. Third, several new mechanistic models now provide quantitative predictions of the spatial structure of the subsurface of the CZ.Many countries fund critical zone observatories (CZOs) to measure the fluxes of solutes, water, energy, gases, and sediments in the CZ and some relate these observations to the histories of those fluxes recorded in landforms, biota, soils, sediments, and rocks. Each US observatory has succeeded in (i) synthesizing research across disciplines into convergent approaches; (ii) providing long-term measurements to compare across sites; (iii) testing and developing models; (iv) collecting and measuring baseline data for comparison to catastrophic events; (v) stimulating new process-based hypotheses; (vi) catalyzing development of new techniques and instrumentation; (vii) informing the public about the CZ; (viii) mentoring students and teaching about emerging multidisciplinary CZ science; and (ix) discovering new insights about the CZ. Many of these activities can only be accomplished with observatories. Here we review the CZO enterprise in the United States and identify how such observatories could operate in the future as a network designed to generate critical scientific insights. Specifically, we recognize the need for the network to study network-level questions, expand the environments under investigation, accommodate both hypothesis testing and monitoring, and involve more stakeholders. We propose a driving question for future CZ science and a hubs-and-campaigns model to address that question and target the CZ as one unit. Only with such integrative efforts will we learn to steward the life-sustaining critical zone now and into the future.
AB - The critical zone (CZ), the dynamic living skin of the Earth, extends from the top of the vegetative canopy through the soil and down to fresh bedrock and the bottom of the groundwater. All humans live in and depend on the CZ. This zone has three co-evolving surfaces: the top of the vegetative canopy, the ground surface, and a deep subsurface below which Earth's materials are unweathered. The network of nine CZ observatories supported by the US National Science Foundation has made advances in three broad areas of CZ research relating to the co-evolving surfaces. First, monitoring has revealed how natural and anthropogenic inputs at the vegetation canopy and ground surface cause subsurface responses in water, regolith structure, minerals, and biotic activity to considerable depths. This response, in turn, impacts aboveground biota and climate. Second, drilling and geophysical imaging now reveal how the deep subsurface of the CZ varies across landscapes, which in turn influences aboveground ecosystems. Third, several new mechanistic models now provide quantitative predictions of the spatial structure of the subsurface of the CZ.Many countries fund critical zone observatories (CZOs) to measure the fluxes of solutes, water, energy, gases, and sediments in the CZ and some relate these observations to the histories of those fluxes recorded in landforms, biota, soils, sediments, and rocks. Each US observatory has succeeded in (i) synthesizing research across disciplines into convergent approaches; (ii) providing long-term measurements to compare across sites; (iii) testing and developing models; (iv) collecting and measuring baseline data for comparison to catastrophic events; (v) stimulating new process-based hypotheses; (vi) catalyzing development of new techniques and instrumentation; (vii) informing the public about the CZ; (viii) mentoring students and teaching about emerging multidisciplinary CZ science; and (ix) discovering new insights about the CZ. Many of these activities can only be accomplished with observatories. Here we review the CZO enterprise in the United States and identify how such observatories could operate in the future as a network designed to generate critical scientific insights. Specifically, we recognize the need for the network to study network-level questions, expand the environments under investigation, accommodate both hypothesis testing and monitoring, and involve more stakeholders. We propose a driving question for future CZ science and a hubs-and-campaigns model to address that question and target the CZ as one unit. Only with such integrative efforts will we learn to steward the life-sustaining critical zone now and into the future.
UR - http://www.scopus.com/inward/record.url?scp=85034602972&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=85034602972&partnerID=8YFLogxK
U2 - 10.5194/esurf-5-841-2017
DO - 10.5194/esurf-5-841-2017
M3 - Article
AN - SCOPUS:85034602972
SN - 2196-6311
VL - 5
SP - 841
EP - 860
JO - Earth Surface Dynamics
JF - Earth Surface Dynamics
IS - 4
ER -