Vegetation Mapping
One
of the future goals of this research is a system of mapping, not
only vegetation by species, but also vegetation communities, so
that the habitat for each endangered species may be determined and
protected. Another long-term research priority is to develop a hydrological
and habitat model of the delta, so the effects of water releases
on the riparian and wetland habitats and the wildlife that use those
areas, can be predicted. Land cover and land use information in
the delta is also needed to target the most productive area for
restoration projects. The need for land cover classes is necessary
to determine the extent and magnitude of land cover change and to
solve a range of environmental problems. Land cover change, especially
the growing extent of agriculture and human settlements, impacts
the habitability of Earth and is fundamental to changes in climate,
carbon and biogeochemical fluxes, hydrologic cycling, surface energy
balance, and the overall functioning of the ecosystem (Townshend
et al., 1991). They showed that traditional classifications are
deficient and conventional methods for collecting ground data are
time-consuming, not easily repeatable, and expensive.
Current mapping systems used for vegetation on the Colorado River
In
the case of the Colorado River, there are two vegetation classifications
used to assess land cover and land use. The first is the Anderson-Ohmart
system and the other is the BoR's Lower Colorado River Accounting
System (LCRAS) (Figure 1, APPENDIX A). The Anderson-Ohmart system
(Ohmart et al., 1988) is based on a series of studies that described
the "community structure" of the riparian corridor from
Davis Dam, below Grand Canyon, to the Southerly International Boundary
at San Luis. Mapping units are approximately 2 ha in area. Using
aerial photography and ground-truthing methods, each map unit is
classified into one of several vegetation types based on the dominant
species. Then, it is classified into one of six vertical complexity
classes based on the proportion of understory, midstory and overstory
vegetation. This sytem purportedly captures the major habitat types
in terms (primarilly) of bird usage. However, it is only semi-quantitative
and cannot be used to actually calculate how many acres of riparian
zone are covered with particular species, such as cottonwoods and
willows.
The LCRAS system, by contrast, relies on satellite
imagery and attempts to be quantitative at least in terms of water
use by crops and phreatophytes along the river (Congalton et al.,
1998). However, the resolution of the TM images on which LCRAS relies
is too low to capture different community types in the riparian
corridor - river vegetation outside the agricualtural areas is simply
lumped together as "phreatophytes". Furthermore, the ET
estimations for phreatophyte vegetation is based on an assumed (untested)
crop coefficient that lumps all plant types together and has only
a single step between summer and winter ET. A new mapping system,
more quantitative than the Anderson-Ohmart system yet containing
biologically significant mapping units, is needed not only for the
delta of the river but for the entire lower Colorado River.
|