Authors: Kyle Cavanaugh*, UCLA - LOS ANGELES, CA
Topics: Global Change, Coastal and Marine, Remote Sensing
Keywords: climate change, range limits, mangroves, remote sensing
Session Type: Paper
Start / End Time: 8:00 AM / 9:40 AM
Room: Jackson, Marriott, 5th Floor
Presentation File: No File Uploaded
Climate change is redistributing species around the globe, and one consequence is a tropicalization of temperate ecosystems. In coastal wetlands along the east coast of North America, there have been observations of mangroves expanding into salt marshes near the current poleward range limit of mangroves in northeast Florida. However, there is currently a debate over whether these changes are a response to anthropogenic climate change (ACC), or are simply reemergences of mangroves in response to decadal-scale oscillations in climate.
We used satellite imagery, aerial photos, historical shoreline maps from the USGS, and other historical records to document changes in mangrove abundance along the northeast coast of Florida from the late 1700s to the present.
We found that these coastal wetlands shifted between mangrove and saltmarsh dominance a number of times over this period. Shifts towards saltmarsh dominance were relatively rapid and linked to extreme freeze events, while shifts towards mangrove dominance occurred during periods of milder winters. We then used modeled climate projections to estimate the contribution of ACC to observed decreases in the frequency of extreme freeze events. We also projected how the frequency of freeze events in this region will change over the next 50 years. Our results suggest that the recent mangrove range expansions should indeed be placed into a broader historical context of an oscillating system. However, this recent expansion may be different than previous ones as it is likely that ACC is causing a more permanent shift towards mangrove dominance in this region.