California Rapid Assessment Method for Wetlands - State Water ...
California Rapid Assessment Method for Wetlands - State Water ...
California Rapid Assessment Method for Wetlands - State Water ...
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<strong>Cali<strong>for</strong>nia</strong> <strong>Rapid</strong> <strong>Assessment</strong> <strong>Method</strong> <strong>for</strong> <strong>Wetlands</strong> v. 5.0.2 – Chapter 4<br />
A<br />
4.6a<br />
A<br />
B<br />
C<br />
B<br />
C<br />
D<br />
D<br />
4.6b<br />
A<br />
A<br />
B<br />
B<br />
C<br />
C<br />
4.6c<br />
D<br />
Figure 4.6: Scale-independent schematic profiles<br />
of Topographic Complexity.<br />
Each profile A-D represents one-half of a<br />
characteristic cross-section through an AA <strong>for</strong><br />
(4.6a) Slope, Playas, Depressional <strong>Wetlands</strong><br />
and Individual Vernal Pools, (4.6b) Estuarine<br />
<strong>Wetlands</strong>, and (4.6c) Lacustrine and Riverine<br />
<strong>Wetlands</strong>. The right end of each profile<br />
represents one edge of the AA. For vernal<br />
pool systems, the right end (4.6a) represents<br />
the lower margin of the upland matrix,<br />
slightly above the edge of a large or small<br />
vernal pool.<br />
Rating<br />
A<br />
B<br />
C<br />
D<br />
Table 4.18a: Rating of Topographic Complexity <strong>for</strong> Depressional <strong>Wetlands</strong>,<br />
Playas, Individual Vernal Pools, and Slope <strong>Wetlands</strong>.<br />
Alternative <strong>State</strong>s<br />
(based on diagrams in Figure 4.6 above)<br />
AA as viewed along a typical cross-section has at least two benches or breaks<br />
in slope, and each of these benches, plus the slopes between them contain<br />
physical patch types or features that contribute to abundant microtopographic<br />
relief or variability as illustrated in profile A of Figure 4.6a.<br />
AA has at least two benches or breaks in slope above the middle area or<br />
bottom zone of the AA, but these benches and slopes mostly lack abundant<br />
micro-topographic relief. The AA resembles profile B of Figure 4.6a.<br />
AA lacks any obvious break in slope or bench, and is best characterized has a<br />
single slope that has at least a moderate amount of micro-topographic<br />
complexity, as illustrated in profile C of Figure 4.6a.<br />
AA has a single, uni<strong>for</strong>m slope with little or no micro-topographic complexity,<br />
as illustrated in profile D of Figure 4.6a.<br />
72