Ecosystem responses to elevated CO<sub>2</sub> using airborne remote sensing at Mammoth Mountain, California
-
Published:2018-12-14
Issue:24
Volume:15
Page:7403-7418
-
ISSN:1726-4189
-
Container-title:Biogeosciences
-
language:en
-
Short-container-title:Biogeosciences
Author:
Cawse-Nicholson KerryORCID, Fisher Joshua B.ORCID, Famiglietti Caroline A., Braverman Amy, Schwandner Florian M.ORCID, Lewicki Jennifer L., Townsend Philip A., Schimel David S.ORCID, Pavlick Ryan, Bormann Kathryn J., Ferraz AntonioORCID, Kang Emily L., Ma PulongORCID, Bogue Robert R., Youmans Thomas, Pieri David C.
Abstract
Abstract. We present an exploratory study examining the use of airborne
remote-sensing observations to detect ecological responses to elevated
CO2 emissions from active volcanic systems. To evaluate these
ecosystem responses, existing spectroscopic, thermal, and lidar data acquired
over forest ecosystems on Mammoth Mountain volcano, California, were
exploited, along with in situ measurements of persistent volcanic soil
CO2 fluxes. The elevated CO2 response was used to
statistically model ecosystem structure, composition, and function, evaluated
via data products including biomass, plant foliar traits and vegetation
indices, and evapotranspiration (ET). Using regression ensemble models, we
found that soil CO2 flux was a significant predictor for ecological
variables, including canopy greenness (normalized vegetation difference
index, NDVI), canopy nitrogen, ET, and biomass. With increasing CO2,
we found a decrease in ET and an increase in canopy nitrogen, both consistent
with theory, suggesting more water- and nutrient-use-efficient canopies.
However, we also observed a decrease in NDVI with increasing CO2 (a
mean NDVI of 0.27 at 200 g m−2 d−1 CO2 reduced to a mean
NDVI of 0.10 at 800 g m−2 d−1 CO2). This is inconsistent
with theory though consistent with increased efficiency of fewer leaves. We
found a decrease in above-ground biomass with increasing CO2, also
inconsistent with theory, but we did also find a decrease in biomass
variance, pointing to a long-term homogenization of structure with elevated
CO2. Additionally, the relationships between ecological variables
changed with elevated CO2, suggesting a shift in coupling/decoupling
among ecosystem structure, composition, and function synergies. For example,
ET and biomass were significantly correlated for areas without elevated
CO2 flux but decoupled with elevated CO2 flux. This study
demonstrates that (a) volcanic systems show great potential as a means to
study the properties of ecosystems and their responses to elevated
CO2 emissions and (b) these ecosystem responses are measurable using a
suite of airborne remotely sensed data.
Publisher
Copernicus GmbH
Subject
Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics
Reference74 articles.
1. Anderson, D. E. and Farrar, C. D.: Eddy covariance measurement of CO2
flux to the atmosphere from an area of high volcanogenic emissions, Mammoth
Mountain, California, Chem. Geol., 177, 31–42, 2001. 2. AVIRIS Data Portal: Jet Propulsion Laboratory, California Institute of Technology, available at: https://aviris.jpl.nasa.gov/alt_locator/, last access: 13 December 2018. 3. Biondi, F. and Fessenden, J. E.: Response of Lodgepole Pine growth to
CO2 degassing at Mammoth Mountain, California, Ecology, 80,
2420–2426, 1999. 4. Boudoire, G., Di Muro, A., Liuzzo, M., Ferrazzini, V., Peltier, A.,
Gurrieri, S., Michon, L., Giudice, G., Kowalski, P., and Boissier, P.: New
perspectives on volcano monitoring in a tropical environment: Continuous
measurements of soil CO2 flux at Piton de la Fournaise (La Réunion
Island, France), Geophys. Res. Lett., 44, 8244–8253, 2017. 5. Camarda, M., De Gregorio, S., and Gurrieri, S.: Magma-ascent processes during
2005–2009 at Mt. Etna inferred by soil CO2 emissions in peripheral
areas of the volcano, Chem. Geol., 330, 218–227, 2012.
Cited by
10 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献
|
|