Section 5: Network-Wide Scoping,
Identification, and Prioritization of Vital Signs for Aquatic Resource
Monitoring
<<
Previous
|
Table of
Contents |
Next
>>
C. Park-Level Vital Signs Tables
Crater Lake National Park (CRLA)
Crater Lake aquatic resources occur within and
outside of the Mt. Mazama caldera. Crater Lake is the focus of most park
visitors, and a long-term monitoring program of lake and inner-caldera streams
and springs water quality has been active since June, 1983. Geothermal sites
deep in Crater Lake are also identified as an important resource within the
caldera. Freshwater resources outside of the caldera include: (1) relatively
small and shallow ponds, lakes, and wetlands; (2) Sphagnum Bog Research Natural
Area; and (3) numerous streams and springs. Vital Signs for Crater Lake,
inner-caldera streams and springs, and lentic systems outside of the caldera, in
order of priority, are: (1) climate change (e.g., temperature and precipitation
regimes); (2) presence and extent of native/introduced (invasive) aquatic biota;
(3) atmospheric deposition of nutrients and pollutants; and (4) visitor use
impacts - recreation and motorized boat use on Crater Lake. Vital Signs for
perennial streams and springs outside of the caldera, in order of priority, are:
(1) presence and extent of native/introduced (invasive) aquatic biota; (2)
atmospheric deposition of nutrients and pollutants; and (3) land and
non-recreational human use impacts – park operations. Cattle trespass is
identified as a potential vital sign of Sphagnum Bog RNA. There is also concern
that geothermal exploration near the CRLA boundary could negatively impact
geothermal sites within the caldera. A detailed summary of Crater Lake aquatic
resource vital signs, potential stress indicators, and associated monitoring
options is presented in Table 14A-D.
Lassen Volcanic National Park (LAVO)
Aquatic resources in Lassen can be grouped into
two categories: (1) ponds and lakes, wetlands, and streams; and (2)
geothermal/hydrothermal features such as hot springs and streams, fumaroles, and
mudpots. Ponds and lakes, wetlands, and streams are grouped together because the
same stressors impact each resource-type. Vital signs of lentic and lotic
resources, in order of priority, are: (1) climate change (e.g., temperature and
precipitation regimes); (2) atmospheric deposition of nutrients and pollutants
(3) presence and extent of native/introduced (invasive) aquatic biota (esp.,
non-native trout and charr); and (4) Visitor use impacts - recreational (e.g.,
hiking, backpacking and camping) and non-recreational (park operations, e.g.,
parking lot and road maintenance, and various construction projects). Visitor
use impacts - recreational is identified as the major vital sign of geothermal/
hydrothermal resources in Lassen. Geothermal/hydrothermal resources have been
and continue to be monitored as part of the USGS Volcano Monitoring Program. A
detailed summary of Lassen aquatic resource vital signs, potential stress
indicators, and associated monitoring options is presented in Table 15AB.
Lava Beds National Monument (LABE)
No permanent surface freshwater resources exist
within the boundaries of Lava Beds; however, a few intermittent-ephemeral ponds
occur. Aquatic resources in Lava Beds occur primarily as ice and water in
permanent ice caves and seasonal wet caves, and groundwater. Stressors of these
resources include reduced precipitation associated with increased air
temperatures and evaporation, and decreased relative humidity in caves. These
changes could subsequently decrease the amount of ice in caves and the
availability of water for Lava Beds biota. Since water is a precious commodity
in Lava Beds, any change in water availability due either to stress of natural
or anthropogenic origin could be quite detrimental to Lava Beds ecosystems.
Stressors of anthropogenic origin include impacts due to climate change,
geothermal exploration, agricultural land use (esp., irrigation and use of
chemicals), and timber harvest just outside of the Lava Beds boundary. The
priority vital signs for Lava Beds aquatic resources are: (1) climate change
(e.g., temperature and precipitation regimes); (2) groundwater; (3) agricultural
chemicals in cave ice and water; and (4) extent of impact on water quality of
activities associated with park unit development, visitor use, and water runoff
from roads. A detailed summary of Lava Beds aquatic resource vital signs,
potential stress indicators, and associated monitoring options is presented in
Table 16A-D.
Oregon Caves National Monument (ORCA)
The aquatic resources of Oregon Caves consist
of an in-cave stream and springs, and surface streams. Stressors to in-cave
resources include: (1) impacts due to climate change; (2) human actions that
modify the cave environment, especially modification of cave openings; (3)
visitor use impairments due to the introduction of inorganic and organic
contaminants; (4) manipulation of the cave environment through the introduction
of artificial light; (5) subsequent increase in algal growth in the cave and the
introduction of contaminants (e.g., bleach) during cave algae control efforts;
and (6) decrease in the amount and availability of in-cave water due to
withdrawal of water from surface streams for fire suppression. Surface streams
are susceptible to the effects of climate change, catastrophic fire, and debris
flows. Cave Creek, a primary stream flowing through Oregon Caves, is also
particularly susceptible to contamination by drain field leaching. The presence
of grazing cattle near Oregon Caves’ streams may also contribute to the
potential contamination of the Oregon Caves water supply. The priority vital
signs of Oregon Caves’ aquatic resources are: (1) drain field contamination of
Cave Creek; (2) cave environment relative to the modified cave opening; (3)
visitor usage; and (4) cave environment relative to introduction of artificial
light. A detailed summary of Oregon Caves’ aquatic resource vital signs,
potential stress indicators, and associated monitoring options is presented in
Table 17A-B.
Redwood National and State Parks (RNSP)
Freshwater and marine aquatic resources are
present in Redwoods. Freshwater resources include impaired streams (i.e.,
Redwood Creek and Klamath River), numerous unimpaired streams (e.g., Godwood
Creek, Hayes Creek, Little Lost Man Creek, Mill Creek, Upper Prairie Creek, and
Smith River), and small ponds and wetlands. Marine resources include the
intertidal and offshore coastal zones, the estuaries of Redwood Creek and
Klamath River, several lagoons (i.e., Espa, Lagoon Creek, and Freshwater), and
coastal ponds at Enderts Beach.
Redwood Creek and Klamath River are listed
under section 303(d) of the Clean Water Act for high water temperature and
unacceptable levels of sedimentation and nutrients (see Table 1). Additional
stressors include: (1) the presence of introduced invasive species; (2) upstream
land use activities (e.g., timber harvest, use of herbicides, and controlled
burns); (3) highway- and levee-related perturbations (e.g., road and culvert
failures, runoff and toxic spills, and levee maintenance); (4) contamination
from septic system leaching and illegal garbage/trash dumping; and (5)
riparian/bank disturbance associated with recreational fishing. Park watershed
rehabilitation activities and inchannel gravel extraction additionally impact
Redwood Creek. The unimpaired sites will be useful for determining baseline
water quality characteristics and range of natural variation of Redwoods
streams. Immediate stressors to these systems include runoff and toxic spills
from State Highway 229 and U.S. Highway 101 and groundwater draw-down at the
Mill Creek Campground.
Stressors affecting marine resources vary
according to resource-type. Intertidal and offshore coastal areas can be
affected by: (1) climate change and climatic events such as El Niņo; (2)
offshore oil spills and the dumping of garbage/plastics; (3) reduced downstream
sediment transport due to the presence of Klamath River dams; and (4) commercial
fishing of smelt and rockfish. Estuaries are affected by changes in hydrology,
increased water temperatures, runoff and spills from US Highway 101, and the
removal and illegal cutting of wood. The Redwood Creek estuary is also impacted
by human activities that degrade riparian habitat, and by dairy farming and
flood control projects. Lagoons and coastal ponds can be stressed by
human-related perturbations associated with road drainage and maintenance, park
development, and potential toxic contamination from an old mill site. The
presence or possible introduction of various non-native invasive species (e.g.,
algae and invertebrates, European beachgrass, and numerous other exotic plants,
etc.) can affect all marine resource-types.
The priority vital signs for Redwoods
freshwater resources are: (1) 303(d) listed streams (Redwood Creek and Klamath
River); (2) upstream land cover and use; (3) recreational fishing; and (4)
presence and extent of introduced exotic biota. The priority vital signs for
Redwoods marine resources are: (1) commercial fishing; (2) extent of impacts on
water quality due to human activities related to flood control and dairy farming
(Redwood Creek only); (3) presence and extent of invasive biota; and (4)
presence and extent of pollutants (e.g., oil) and garbage/plastics offshore and
on beaches. A detailed summary of Redwoods aquatic resource vital signs,
potential stress indicators, and associated monitoring options is presented in
Tables 18A-C and 19A-C.
Whiskeytown National Recreation Area (WHIS)
Whiskeytown aquatic resources include
Whiskeytown Lake, perennial streams, mineral springs, permanent and intermittent
small-shallow ponds, and marshes. Water related activities (e.g., boating,
sailing, water skiing, kayaking, swimming, fishing, etc.) are the primary
recreational focus of visitors to Whiskeytown Lake and are potential stressors
of reservoir water quality. Additional stressors related to human activity
include: park unit sewage treatment and wastewater discharge by surrounding
communities; marijuana farming and heavy metals contamination from past mining
operations on the upstream sections of reservoir tributaries; and water level
fluctuations caused by reservoir dam operations. As is the case with many large
water bodies in the western USA, the introduction of non-native invasive floral
and faunal species impact the native biota of Whiskeytown Lake. Impacted
perennial streams have been affected by human-related activity (e.g., past
mining operations; treatment and disposal of human waste; marijuana farming;
recreation; deteriorating abandoned logging roads; gravel injection and waste
rock disposal; prescribed/natural fires and related activities; floods; and
introduced nonnative invasive biota). The unimpaired perennial streams in
Whiskeytown can be used to determine baseline lotic water quality conditions and
range of natural variation. However, these streams can also be affected by
perturbations of natural and anthropogenic origin. Whiskeytown also contains a
complex of mineral springs that supports a small, indigenous population of
Howell’s alkali grass (Puccinellia howellii), which is listed by the California
Native Plant Society as rare and endangered. Stressors to this resource include:
(1) littering and garbage dumping, trampling, and off-road vehicle use); (2)
change in hydrology; (3) State Highway 299 maintenance and
contamination/pollution due to vehicle use and accidents; and (4) potential
invasion by saltgrass (Distichlis spicata). Little is known about the various
permanent and intermittent small-shallow ponds and marshes that occur in
Whiskeytown. They, like the unimpaired perennial streams, are susceptible to
various types of stress of natural and anthropogenic origin. The priority vital
signs of Whiskeytown aquatic resources are: (1) extent of human impacts such as
heavy metals contamination associated with from past mine operations and
tailings; (2a) park unit sewage treatment and disposal; (2b) septic tanks,
garbage/trash, and marijuana farming; and (3) extent and occurrence of natural
and prescribed fire. A detailed summary of Whiskeytown aquatic resource vital
signs, potential stress indicators, and associated monitoring options is
presented in Table 20AE.
| Table 14: Crater
Lake National Park Vital Signs Tables |
| A: Crater Lake and inner-caldera streams and
springs; ponds, lakes and wetlands outside of caldera Priority Vital Sign
Potential Stress Indicators Potential Monitoring Options |
 |
| B: Sphagnum Bog
Research Natural Area |
 |
| C: Perennial
streams and springs outside of the caldera. |
 |
| D: Subsurface geothermal sites in Crater Lake |
 |
| Table 15: Lassen
Volcanic National Park Vital Signs Tables |
| A: Ponds, lakes, wetlands and perennial streams |
 |
| B: Geothermal/hydrothermal |
 |
| Table 16: Lava
Beds National Monument Vital Signs Tables |
| A: Permanent ice caves |
 |
| B: Seasonal ice caves |
 |
| C: Intermittent ephemeral ponds |
 |
| D: Groundwater |
 |
| Table 17: Oregon
Caves National Monument Vital Signs Tables |
| A: In-cave stream and springs |
 |
| B: Perennial surface streams |
 |
| Table 18: Redwood
National and State Parks Vital Signs Tables
(Freshwater) |
| A: Impaired perennial streams (Redwood Creek
and Klamath River) |
 |
| B: Unimpaired perennial streams (e.g., Godwood,
Upper Prairie, and Hayes Creeks; Smith River) |
 |
| C: Freshwater ponds and wetlands (Marshall
Pond, small ponds at Gold Bluffs Beach) |
 |
| Table 19: Redwood
National and State Parks Vital Signs Table (Marine) |
| A: Intertidal and offshore coastal |
 |
| B: Lagoons (Espa, Lagoon Creek, Enderts Beach
pond) |
 |
| C: Estuaries (Redwood Creek, Klamath River) |
 |
| Table 20: Whiskeytown
National Recreation Area Vital Signs Tables |
| A: Whiskeytown Lake (Reservoir) |
 |
| B: Impaired perennial streams |
 |
| C: Unimpaired perennial streams |
 |
| D: Complex of mineral springs and Howell’s
alkali grass (Puccinellia howellii) |
 |
| E: Permanent small-shallow ponds, intermittent
ephemeral ponds, marshes |
 |