refine and integrate linked hydrological/ecological models with remote sensing products: leaf area...
TRANSCRIPT
Refine and integrate linked hydrological/ecological models with remote sensing products: leaf area index, wetland maps, seasonal flooding, water boundaries and soil moisture.
Motivation & Research Questions
Invasive plants in coastal wetlands of the Great Lakes are degrading wetland habitat, decreasing biodiversity and
reducing ecosystem services.
How will climate and land use change influence the spread and impact of invasive plant species?
What are the mechanisms that govern their spread so that actions can be taken to reduce damage?
Monitoring and Modeling the vulnerability of coastal Great Lakes wetlands to climate change and land use
Laura Louise Bourgeau-Chavez
Research Team
Laura Bourgeau-Chavez Michigan Tech Research InstituteMichigan Technological University3600 Green Court, Suite 100Ann Arbor, MI 48105(734) [email protected]
Nancy H F French, PhD, & Mary Ellen Miller, PhD, &Liza Jenkins Michigan Tech Research InstituteMichigan Technological UniversityAnn Arbor, MI
Deborah Goldberg, PhD, &Kenneth Elgersma, PhDDept. of Ecology & Evolutionary BiologyUniversity of MichiganAnn Arbor, MI
David Hyndman , PhD, &Anthony D Kendall, PhDDept. of Geological SciencesMichigan State UniversityEast Lansing, MI
William Currie, PhDSchool of Natural Resources & EnvironmentUniversity of MichiganAnn Arbor, MI
Study invasive species (Phragmites australis, Typha angustifolia, Typha x glauca) and their native counterparts in small controlled enclosures in the natural environment.
Simulate changes in upland land use and climate in order to understand the impacts of changing water and nutrient loads on coastal ecosystems.
Remote Sensing to parameterizeand improve linked models
Coupling Ecological and Hydrological models
Mesocosms of invasivewetland plant species
F ig. 1 : C o nc e p tu a l c o nne c tio ns b e tw e e n e xis ting hy d ro lo gy a nd e c o s y s te m m o d e ls .
Hy drology
C limateC limate
InvasionNutr ient f lux,temperature
Land use
Biodiversity
N retention
Csequestration
U P LA N D W A T E R S H E D W E T LA N D
ILH M M o ndrian
Nutr ient f lux
In va sio n
Bio d ive rs ity
Nu tr ien t
Urbanization
W a te r
Flux Mondrian: Modes Of Nonlinear Dynamics in Resource
Interactions And Nutrient cycling. A wetland ecosystem model capable of predicting ecosystem responses to changing conditions.
ILHM: The Integrated Landscape Hydrology Model. A process based hydrological model enhanced to predict water and nutrient transport.
(a) 0.53 g invader, N inflow = 2.5 g N / m2 y
-5 0 5 10 15 20 25
No
rm
alize
d N
PP
a
nd
N
u
pta
ke
0.0
0.2
0.4
0.6
0.8
1.0
1.2
NPP of invaderN uptake
-5 0 5 10 15 20 25
No
rm
alize
d N
PP
a
nd
N
u
pta
ke
0.0
0.2
0.4
0.6
0.8
1.0
1.2
(b) 0.53 g invader, N inflow = 9.0 g N / m2 y
-5 0 5 10 15 20 25
No
rm
alize
d N
PP
a
nd
N
u
pta
ke
0.0
0.2
0.4
0.6
0.8
1.0
1.2
(c) 5.3 g invader, N inflow = 2.5 g N / m2 y
Years
-5 0 5 10 15 20 25
No
rm
alize
d N
PP
a
nd
N
u
pta
ke
0.0
0.2
0.4
0.6
0.8
1.0
1.2
(d) 5.3 g invader, N inflow = 9.0 g N / m2 y
Mondrian model results showing a time series of attempted invasions into established native communities over time; the x-axis shows time (years) since start of attempted invasion. The y-axis shows NPP of the invader species as a proportion of total community NPP, together with community-aggregated flux of N uptake into plants, normalized to a 0-1 scale relative to the ending value in panel (d). Combinations of invader size and N inflow fluxes are listed on each panel.
Map Leaf Area Index (LAI) using MODIS LUT algorithms and\or vegetation indices (WDVI, EVI, NDVI). The LAI is an important driver for hydrologic and biophysical modeling because canopies intercept precipitation, affect NPP (Net Primary Production), shade the ground below, and are linked to root water uptake.
Map seasonally saturated and inundated soils with L- and C- band SAR data. These maps used in conjunction with DEM data will provide a better understanding of “internally drained areas” than could be obtained by topographic data alone. Field campaigns will be undertaken to validate soil moisture and map extents of “internally drained areas”.
Map wetland vegetation cover type in coastal regions of Michigan’s lower peninsula using a fusion of multi-date and multi-sensor SAR and Optical data. These maps will be used to assess predictions of invasion spread and wetland species composition.
Landsat data: Traverse City, MI 5/16/10
6/17/10
10/7/10
Envisat data: Traverse City, MI 5/22/11
Phragmites australis
(a) 0.53 g invader, N inflow = 2.5 g N / m2 y
-5 0 5 10 15 20 25
No
rm
alize
d N
PP
a
nd
N
u
pta
ke
0.0
0.2
0.4
0.6
0.8
1.0
1.2
NPP of invaderN uptake
-5 0 5 10 15 20 25
No
rm
alize
d N
PP
a
nd
N
u
pta
ke
0.0
0.2
0.4
0.6
0.8
1.0
1.2
(b) 0.53 g invader, N inflow = 9.0 g N / m2 y
-5 0 5 10 15 20 25
No
rm
alize
d N
PP
a
nd
N
u
pta
ke
0.0
0.2
0.4
0.6
0.8
1.0
1.2
(c) 5.3 g invader, N inflow = 2.5 g N / m2 y
Years
-5 0 5 10 15 20 25
No
rm
alize
d N
PP
a
nd
N
u
pta
ke
0.0
0.2
0.4
0.6
0.8
1.0
1.2
(d) 5.3 g invader, N inflow = 9.0 g N / m2 y
(a ) 0 .5 3 g in v a d e r , N in f lo w = 2 .5 g N / m 2 y
-5 0 5 10 15 20 25
No
rm
aliz
ed
N
PP
a
nd
N
u
pta
ke
0 .0
0 .2
0.4
0.6
0.8
1.0
1.2
N P P of invader
N uptake
-5 0 5 10 15 20 25
No
rm
aliz
ed
N
PP
a
nd
N
u
pta
ke
0 .0
0 .2
0.4
0.6
0.8
1.0
1.2
(b ) 0 .5 3 g in v a d e r , N in f lo w = 9 .0 g N / m 2 y
-5 0 5 10 15 20 25
No
rm
aliz
ed
N
PP
a
nd
N
u
pta
ke
0 .0
0 .2
0.4
0.6
0.8
1.0
1.2
(c ) 5 .3 g in v a d e r , N in f lo w = 2 .5 g N / m 2 y
Y e a rs
-5 0 5 10 15 20 25
No
rm
aliz
ed
N
PP
a
nd
N
u
pta
ke
0 .0
0 .2
0.4
0.6
0.8
1.0
1.2
(d ) 5 .3 g in v a d e r , N in f lo w = 9 .0 g N / m 2 y
Typha latifolia
Leaf Area Index is the area of one side of each leaf per unit area of ground.