Mark Steffen 02-12-08
Federation of Fly Fishers/Northern Arizona Flycasters (FFF/NAF)
Regarding: Reclamation Environmental Assessment, Experimental releases from Glen Canyon Dam, Arizona, 2008 through 2012.
I STRONGLY OPPOSE THE RECLAMATION PROPOSED EXPERIMENTS, THE HIGH TEST FLOW AND THE FALL STEADY FLOWS!
I STRONGLY SUPPORT THE “NO ACTION ALTERNATIVE”, and offer the following comments:
It is unfortunate that Reclamation and the Department of the Interior, including the National Park Service (NPS) and the US Fish and Wildlife Service (FWS) have chosen to force these experiments on the public with a complete lack of consideration and in defiance of five years of collaboration by Stakeholders in the Glen Canyon Dam Adaptive Management Program (GCDAMP). Stakeholders including FFF/NAF worked hard to design appropriate flow experiments, only to be forced now to accept these Bureau of Reclamation experiments which were repeatedly voted down by GCDAMP Stakeholders.
Grand Canyon Monitoring and Research Center (GCMRC) scientists, Reclamation bureaucrats, the NPS, the FWS and the Grand Canyon Trust wear rose colored glasses and assume that high flows and steady flows will be a panacea for all resources downstream of Glen Canyon Dam. This is an outrageously fallacious, dangerous and irresponsible assumption that ignores the negative consequences of all past grandiose, extreme flow experiments that have had disastrous impacts on the aquatic ecosystem in a fanatical, zealous and blind obsession to manipulate sand in the Grand Canyon.
The comment period of 14 days is grossly inadequate and irresponsible for experiments this extreme, this excessive, this expensive and this controversial. Notification of the public for comments was extremely inadequate. Reclamation in an EA press release seeking comments, did not even give instructions on how the public should submit comments.
IMPACTS TO FISH AND FISH FOOD SUPPLIES:
1) The Little Colorado River (LCR) flooded in Late January and early February 2008 with a peak flow of 4,400 cfs. This flooding above the base flow of 200cfs certainly flushed many if not most of the young humpback chubs (HBC) born in 2007 in the LCR into the main Colorado River. The USFWS documented this during flooding of the LCR in January and March 2005 (2005 LCR spring trip report Van Haverbeke). The presence of huge numbers of the 2007 HBC LCR year class in the Colorado River should be considered before implementation of a flood flow that would be 3 times the usual March flow. Independent “Science Advisors” have cautioned against doing a test flood shortly after serious flooding from the LCR (Barron, Garret etal 2008). Nonetheless, GCMRC predicts impacts to HBC will be “minimal” (GCMRC 2008).
2) Reclamation admits in the Biological Assessment that the “high flow test” will have negative consequences to humpback chubs. Page 90, “The proposed action is likely to adversely affect humpback chubs” (Reclamation 12-2007).
3) GCMRC does not have the capability to document high test flow affects or steady flow affects on aquatic plants, aquatic insects and food supplies for fish. GCMRC does not have an Aquatic Food Base (AFB) Monitoring program. GCMRC has a “research program” intended to eventually lead to an AFB monitoring program sometime in the far distant future. GCMRC has been repeatedly criticized by independent scientist reviews for a lack of “integration” of physical and biological studies and having too much focus on studying sand and camping beaches.
4) This Reclamation EA misrepresents the concerns of Lees Ferry business owners and fishing guides (EA page 12). Concerns were not just for negative economic impacts and negative public perceptions. A main concern was the damage to aquatic plants and aquatic insects that did occur during the 2004 high flow test. That damage was not documented by GCMRC because they did not have and they still do not have an Aquatic Food Base Monitoring program. Anglers and Lees ferry business owners recommended a high test experiment be conducted in January or July, high water months when the high flow would be relatively less drastic; impacts to the aquatic ecosystem might be less severe and the test would not be in the prime fishing season of early February to late June. Also suggested but ignored in the EA, was stocking trout at Lees Ferry to mitigate possible trout impacts from the high flow and to change the current public perception that trout cannot be stocked at Lees ferry anymore (Steffen 2007). Grand Canyon River guides representative John O Brian stated at a TWG meeting that rafters would not oppose a high flow test in July, that they would enjoy rafting the high water.
5) The No Action Alternative (modified low fluctuating flows) and the cold water released from Glen Canyon Dam have been effective at protecting the Little Colorado River (the spring fed and all year round warm water home of HBC in Grand Canyon) from invasion of warm water non-native fish (channel catfish, small mouth bass, stripped bass etc.) from Lake Mead. This current Reclamation fall steady flow proposal that “might” benefit juvenile HBC by warming backwaters in the Colorado River, also will invite invasion of warm water non-native predacious fish from Lake Mead. These warm water non-native fish would be likely to enter the LCR and could exterminate all remaining HBC in the Grand Canyon. The past four years of government trout killing in the Colorado River has opened a niche and led to increases of existing non-native warm water fish (bullhead catfish and carp) in the Grand Canyon and perhaps in the LCR. Trout in the Colorado River almost never enter the LCR. After 1950 but prior to Glen Canyon Dam, highly predacious catfish were the dominant fish in Grand Canyon (Webb, Melis and Valdez, 2002) and would likely have led to extermination of HBC in Grand Canyon including the LCR. Cold water from Glen Canyon Dam and the No Action Alternative have protected and saved HBC in the Little Colorado River in Grand Canyon. The current Reclamation proposed steady flow experiment creates new threats to the Grand Canyon Little Colorado River HBC population that should not be acceptable.
HIGH FLOW TEST TIMING, MAGNITUDE AND DURATION:
6) There is no need for “expediting” a high flow test (page 6 EA). GCMRC has stated that the current enriched sediment condition will persist in the river for several years (Steffen 2007). A high flow test during a low water month is inappropriate. Damage to the aquatic ecosystem would be much less if the test occurred during a high water month such as January or July.
7) Cladophora (aquatic algae) grows intensely in spring and fall with sharp decreases in mid-summer. Increased growth of Cladophora in spring coincided with rising base flow. (Pinney 1991)
GCMRC has not justified a need for the test flow duration as excessive as the 60 hours in the current Reclamation proposal. The GCMRC science plan does not consider the impact a 60 hour duration 41,000 cfs flow relative to the normal high flow of 13,000cfs, will have on the Aquatic Food Base (GCMRC 2007).
ADVICE IGNORED BY RECLAMATION:
9) The Federation of Fly Fishers and the Northern Arizona Flycasters are listed in the EA as having been consulted. ALL advice give by these organizations was ignored!
10) The Glen Canyon Dam Adaptive Management Work Group (AMWG) has not recommended a high flow test or steady flows. The Glen Canyon Dam Adaptive Management Technical Work Group (TWG) voted not to recommend an identical high flow test proposed by the Grand Canyon Trust in November 2007. The AMWG and TWG have repeatedly voted not to recommend any periods of steady flows.
11) In this EA, Reclamation continues to ignore advice from AMWG and TWG including AFB experiments proposed by WAPA and the Federation of Fly Fishers (FFF) to determine AFB impacts from fluctuating flows and steady flows. Experiments proposed by WAPA and FFF included brief but significant daily flow fluctuations that would attenuate to steady flows 60 miles downstream by the Little Colorado River and chub locations.
12) The expense of this test is grossly excessive. A total cost of twelve million dollars for benefits that will be minimal, maybe only to some camping beaches and to scientist’s resumes (academic reports, graduate degree dissertations etc.).
BACKWATERS:
13) Backwaters are less than 5% of shoreline according to GCMRC data. Backwaters could be destroyed by a high flow. Vegetated shorelines are more important for chubs and may also be destroyed by high flow.
14) IF backwaters are improved even temporarily for chubs, the timing of the test in March will not benefit chubs. A test in July would produce the hypothetical improvement when chubs are actually flushed from the LCR, in July and August by monsoon rains.
STEADY FLOW ISSUES:
15) Steady flows in October will lead to colder, not warmer water temperatures in backwater areas, due to low air temperatures in October, negating and reversing the intent of creating warm backwaters. Fluctuating flows maintain a relatively warm temperature of 50 degrees Fahrenheit in backwater areas even in winter when steady flows would result in very cold shoreline water temperatures.
16) Steady flows would exacerbate the effect of low dissolved oxygen that can occur in fall. Fluctuations increase dissolved oxygen in dam water releases.
17) Reclamation and this EA irresponsibly disregard evidence of benefits and even dependence of aquatic plants, aquatic insects and fish, on daily fluctuating flows. The Colorado River Aquatic Ecosystem (CRE) has evolved, adapted and become dependent on daily flow fluctuations. The CRE is now essentially a “tidal” or “estuarial” ecosystem. Steady flows would be extremely disruptive and analogous to government bureaucrats proposing that some particular ocean organism would benefit if the government could only stop the ocean tides!
18) Cessation of fluctuating flows would likely reduce drifting simmulids, gammarus (fresh water shrimp) and chironomids, important food sources for HBC. Cladophora (aquatic algae) drift was significantly higher during upramp and downramp than during steady flows. Gammarus composed the bulk of HBC diet by volume, although simmulids were the most common by number. (Valdez 1995)
19) Fluctuating flows increase the availability of food, increasing the dislodgement and movement of algae and invertebrates. Invertebrates in trout stomachs increased during periods of fluctuating flow. Anglers favor fluctuating flows because they believe rising water stimulates feeding by fish. Trout growth rates could decline due to an absence of fluctuating flows. (GCES final report introduction January 1988)
20) Fluctuating flows can lead to increased diversity of diatoms that produce mucilage which protects Cladophora against effects of dessication from dewatering during fluctuating flows. (Peterson 1984)
21) Cladophora is conditioned evolutionarily for the submergence-emergence of fluctuating flows in regulated rivers. (Pinney 1991)
22) Cladophora composed 77% of HBC stomach contents in the 1980’s, chironomids and terrestrial insects only 10%. (Kubly 1990)
23) Cladophora was heavily exploited by carp, trout, channel catfish, flannelmouth and bluehead suckers. Oil droplets from diatoms attached to Cladophora provide a major energy source for fish. (Carothers and Minkley 1981)
24) Cladophora and associated diatoms are the foundation of the aquatic food web and are utilized by both Gammarus and Rainbow Trout in Glen Canyon. (Pinney1991)
25) Diatoms associated with Cladophora provide 95% of Gammarus diet at Lees Ferry. Gammarus grazed on diatoms without ingesting the host Cladophora. (Pinney 1991)
26) Diatoms associated with Cladophora appear to be an important food source for Trout below Glen Canyon Dam. Trout derive nutritional benefit from diatom lipids and achieve increased digestive efficiency from a full stomach of indigestible Cladophora. . (Liebfried 1988)
27) Gammarus show a preference for ingesting diatoms that grow best on Cladophora during fluctuating flows versus diatoms that grow under steady flows. Achnanthes affinis-minutissima and Rhoicosphenia curvata versus Cocconeis pediculus. Gammarus had difficulty removing and ingesting the diatom pediculus from cladophora. Pediculus increased with steady flows and decreased with fluctuating flows. Ingestion of A. affinis was high during fluctuating flows and affinis exhibits “hitch hiking” ability on drifting Cladophora. (Pinney 1991)
28) Gammarus become mobile during fluctuating flows. (Pinney 1991)
29) Stomachs of HBC from the Colorado River contained more food than HBC from the Little Colorado River. (Minckley 1996)
Literature cited:
Barron, Dale, Fowler, Gunderson, Kitchell, Robertson, Tyus, Wohl and Garrett.
1-13-2008. Review of the “Science Plan for Potential 2008 Experimental High Flow at Glen Canyon Dam”.
GCMRC, 12-27-2007. Science Plan for Potential 2008 Experimental High Flow at Glen Canyon Dam.
GCMRC, 1-13-2008. GCMRC responses to SA comments on Science Plan for Potential 2008 Experimental High Flow.
Kubly, 1990.The endangered humpback chub in Arizona.
Liebfried and Blinn, 1986 The effects of steady versus fluctuating flow below Glen Canyon Dam.GCES report B-8
Liebfried,1988. The utilization of Cladophora and diatoms as a food resource by Trout in the Colorado river below Glen Canyon Dam.
Minckley, 1996. Observations on the biology of the HBC in the CR basin 1908-1990.
Peterson, 1984. Benthic diatom community dynamics in the Colorado river: Interactive effects of periodic dessication.
Pinney, 1991. The response of Cladophora and associated diatoms to regulated flow, and the diet of Gammarus, in the tailwaters of glen canyon Dam.
Reclamation, 12-2007. Biological Assessment on the Operation of Glen Canyon Dam and Proposed Experimental Flows for the Colorado River Below Glen Canyon Dam During the Years 2008-20012.
Steffen, 12-02-2007. Report on Lees Ferry meeting about 2008 Beach-habitat-building-flow.
Valdez, 1995 Life History and Ecology of the Humpback Chub in the Colorado River, Grand Canyon, Arizona.
Van Haverbeke, USFWS, May 2005. Monitoring of Native Fishes of the Little Colorado River Ecosystem in Grand Canyon. Spring 2005 trip report.
Webb, Melis and Valdez, 2002. Observations of Environmental Change in Grand Canyon, Arizona.
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