TY - JOUR
T1 - Approximations of stand water use versus evapotranspiration from three mangrove forests in southwest Florida, USA
AU - Krauss, Ken W.
AU - Barr, Jordan G.
AU - Engel, Vic
AU - Fuentes, Jose D.
AU - Wang, Hongqing
N1 - Funding Information:
We thank Jim L. Chambers, P. Joy Young, Thomas W. Doyle, Robert R. Twilley, Jason K. Sullivan, and Victor H. Rivera-Monroy for critical collaborations at various stages of this research, and Daniel L. McLaughlin and two anonymous referees for providing comments on previous manuscript drafts. This research was supported by the USGS Priority Ecosystems Program , NPS Critical Ecosystems Initiative (CESI) , USGS Climate and Land Use Change R&D Program , and USGS Ecosystems Mission Area . The National Science Foundation provided support for the analyses associated with the Shark River flux tower data set (award WSC-0920504). Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the US Government.
Publisher Copyright:
© 2014.
PY - 2015/11/1
Y1 - 2015/11/1
N2 - Leaves from mangrove forests are often considered efficient in the use of water during photosynthesis, but less is known about whole-tree and stand-level water use strategies. Are mangrove forests as conservative in water use as experimental studies on seedlings imply? Here, we apply a simple model to estimate stand water use (S), determine the contribution of S to evapotranspiration (ET), and approximate the distribution of S versus ET over annual cycles for three mangrove forests in southwest Florida, USA. The value of S ranged from 350 to 511mmyear-1 for two mangrove forests in Rookery Bay to 872mmyear-1 for a mangrove forest along the Shark River in Everglades National Park. This represents 34-49% of ET for Rookery Bay mangroves, a rather conservative rate of S, and 63-66% of ET for the Shark River mangroves, a less conservative rate of S. However, variability in estimates of S in mangroves is high enough to require additional study on the spatial changes related to forest structural shifts, different tidal regimes, and variable site-specific salinity concentrations in multiple mangrove forests before a true account of water use conservation strategies can be understood at the landscape scale. Evidence does suggest that large, well-developed mangrove forests have the potential to contribute considerably to the ET balance; however, regionally most mangrove forests are much smaller in stature in Florida and likely contribute less to regional water losses through stand-level transpiration.
AB - Leaves from mangrove forests are often considered efficient in the use of water during photosynthesis, but less is known about whole-tree and stand-level water use strategies. Are mangrove forests as conservative in water use as experimental studies on seedlings imply? Here, we apply a simple model to estimate stand water use (S), determine the contribution of S to evapotranspiration (ET), and approximate the distribution of S versus ET over annual cycles for three mangrove forests in southwest Florida, USA. The value of S ranged from 350 to 511mmyear-1 for two mangrove forests in Rookery Bay to 872mmyear-1 for a mangrove forest along the Shark River in Everglades National Park. This represents 34-49% of ET for Rookery Bay mangroves, a rather conservative rate of S, and 63-66% of ET for the Shark River mangroves, a less conservative rate of S. However, variability in estimates of S in mangroves is high enough to require additional study on the spatial changes related to forest structural shifts, different tidal regimes, and variable site-specific salinity concentrations in multiple mangrove forests before a true account of water use conservation strategies can be understood at the landscape scale. Evidence does suggest that large, well-developed mangrove forests have the potential to contribute considerably to the ET balance; however, regionally most mangrove forests are much smaller in stature in Florida and likely contribute less to regional water losses through stand-level transpiration.
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U2 - 10.1016/j.agrformet.2014.11.014
DO - 10.1016/j.agrformet.2014.11.014
M3 - Article
AN - SCOPUS:84940450463
SN - 0168-1923
VL - 213
SP - 291
EP - 303
JO - Agricultural and Forest Meteorology
JF - Agricultural and Forest Meteorology
ER -