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YKL REA Aquatics Becky Shaftel, Leah Kenney, and Timm Nawrocki Aquatics in the REA Conservation elements Distribution mapping methods and results Conceptual models Management questions Aquatic conservation elements Coarse filters • Streams and rivers • Connected lakes • Disconnected lakes Fine filters • Chinook salmon • Chum salmon • Sheefish • Dolly Varden • Northern pike Photo: ADF&G Photo: ADF&G Streams and rivers Methods: flowlines from the USGS National Hydrography Dataset Results: Length = 454,000 km Connected lakes Methods: waterbodies connected to flowlines in the National Hydrography Dataset Results: Count = 31,600 lakes Area = 25,800 km2 Photo: USFWS Disconnected lakes Methods: waterbodies not connected to flowlines in the National Hydrography Dataset Results: Count = 103,600 lakes Area = 9,400 km2 Photo: USFWS Chinook Salmon Methods: Clipped from the Anadromous Waters Catalog event feature class Results: AWC Life Stage Designation Spawning Habitat Present or Rearing Length (km) 5,436 13,522 Photo: USFWS Chum Salmon Methods: Clipped from the Anadromous Waters Catalog event feature class Results: AWC Life Stage Designation Spawning Habitat Present or Rearing Length (km) 5,902 8,640 Photo: USFWS Sheefish Methods: Clipped from the Anadromous Waters Catalog event feature class Results: AWC Life Stage Designation Spawning Habitat Present Length (km) 117 6,036 Photo: USFWS Fish Distribution Models ADF&G AFFID species occurrence data Process AFFID data for use in models GIS source data Create stream network and landscape predictor variables in GIS Fish distributions Predict species habitat across REA study area Classification tree and random forest models Evaluate model performance Photo: USFWS Stream Network Used TauDEM to process DEM 1. Add in additional HUCs on boundary of study area that flow into the study area 2. Fill pits 3. Calculate flow direction (D8 method) 4. Calculate contributing area 5. Create stream network based on curvature method and drop analysis Predictor Variables Predictors of Fish Habitat Elevation Permafrost Gradient Slope over area ratio Stream order Watershed area Average watershed annual precipitation Average watershed annual temperature Average watershed elevation Average watershed slope over area ratio Average watershed slope Percent permafrost cover in watershed Photo: USFWS Percent lake cover in watershed Process AFFID data - - - - Select all presences by fish in AFFID Select absences from projects in AFFID that listed fish community sampling as an objective Resample data in areas of high intensity to match densities in other HUCs Shift points along flow direction grid until they reached the stream network Extract all predictor variables to each data point for model development Classification Trees Asterospicularia laurae Classification Tree Analysis Steps: – Identify the groups – Choose the variables – Identify the split that maximizes the homogeneity of the resulting groups – Determine a stopping point for the tree – Prune the tree using cross-validation Shelf: Inner, Mid Absent 0.97 (263) Shelf: Outer Location: Back, Flank Absent 0.78 (64) (De'Ath and Fabricious 2000) Location: Front Depth < 3m Absent 0.56 (9) Depth ≥ 3m Present 0.81 (37) Misclassification rates: Null = 15%, Model = 9% Photo: USFWS Random Forests Creates many classification trees and combines predictions from all of them: - Start with bootstrapped samples of data - Observations not included are called out-of-bag (OOB) - Fit a classification tree to each bootstrap sample, for each node, use a subset of the predictor variables. - Determine the predicted class for each observation based on majority vote of OOB predictions - To determine variable importance, compare misclassification rates for OOB observations using true and randomly permuted data for each predictor Run models in R ct1<-mvpart(pres.f~.,data=fish.pred1[s1,],xv="1se") rf1<-randomForest(pres.f~.,data=fish.pred1[s1,],ntree=999) CT training CT validation RF training RF validation 1 0.271 0.327 0.248 0.264 2 0.273 0.27 0.262 0.226 3 0.265 0.264 0.24 0.245 4 0.271 0.358 0.238 0.233 5 0.271 0.264 0.251 0.252 6 0.283 0.352 0.257 0.239 7 0.292 0.321 0.249 0.258 8 0.214 0.302 0.246 0.226 9 0.244 0.252 0.265 0.214 Photo: USFWS 10 0.297 0.296 0.267 0.245 summary 0.2681 0.3006 0.2523 0.2402 Model Performance 0 1 Confusion Matrix 0 1 Error 313 96 23.5% 98 282 25.8% Photo: USFWS Dolly Varden Results: ~ 32,000 km of predicted summer habitat (restricted to stream reaches > 1 km in length) Predictor 1 0 watershed 541 m 299 m elevation watershed slope 22% 10% watershed 596 mm 521 mm annual precip. watershed -1.36 C -1.41 C annual temp. Watershed area 71 km2 1,665 km2 Photo: USFWS Increased potential for establishment of invasive macrophytes and changing fire dynamics Direct population decline Permafrost Reduction in juvenile fitness; bioaccumulation in adults Increase in ground flow; increase in sedimentation Reduction in age at maturity and shift in spawning season Fish species Change Agents Drivers CE General Effect Habitat Temporary increases in nutrient inputs; increase sedimentatitation Harvest Reduction in habitat Infrastructure Increased toxicity Contaminants Fire Mining Habitat loss, changes in migration routes, increased sedimentation Increased contaminant sources Change in deposition rates Precipitation Changes in hydrology Expanded ice-free season Permafrost thaw Temperature Invasive Macrophytes Human Uses Climate Change Expanded ice-free season Permafrost Change Agents Drivers CE General Effect CE-Specific Effect Increase groundwater flow improves overwinter habitat Contaminants Infrastructure Harvest Increased toxicity Invasive Macrophytes Reduction in age at maturity and shift in spawning season Dolly Varden Salvelinus malma Habitat Temporary increases in nutrient inputs Human Uses Elodea spp could reduce quality of foraging habitat Direct destruction of habitat, hindrance of migration routes, increased downstream turbidity and sedimentation Climate Change Direct population decline Increased contaminant sources Precipitation Reduction in juvenile fitness; bioaccumulation in adults Temperature Increased winter precipitation may increase overwintering habitat Change in deposition rates Permafrost thaw Increased potential for establishment of invasive macrophytes and changing fire dynamics Fire Mining Expanded ice-free season Permafrost Change Agents Drivers CE General Effect CE-Specific Effect Increase depth of active layer will increase lake drainage area Infrastructure Harvest In creased toxicity Contaminants Invasive Macrophytes Reduction in age at maturity and shift in spawning season Northern Pike Esox lucius Habitat Temporary increases in nutrient inputs Human Uses Elodea ssp could reduce quality of spawning habitat Direct destruction of habitat, hindrance of migration routes, increased downstream turbidity and sedimentation Climate Change Subsistence harvest pressures on overwintering populations Increased contaminant sources Precipitation Bioaccumulation of mercury in adults Temperature Increased winter precipitation may increase overwintering habitat Change in deposition rates Permafrost thaw Increased potential for establishment of invasive macrophytes and changing fire dynamics Fire Mining Expanded ice-free season Sedimentation of gravelsubstrate will reduce quality of spawning habitat Permafrost Change Agents Drivers CE General Effect CE-Specific Effect Infrastructure Harvest In creased toxicity Contaminants Invasive Macrophytes Mining Sheefish Stenodus leucichthys Habitat Sedimentation of gravel-substrate in streams will reduce quality of spawning habitat Reduction in age at maturity and shift in spawning season to later Reduction in juvenile feeding habitat Human Uses Direct destruction of habitat, hindrance of migration routes, increased downstream turbidity and sedimentation Climate Change Direct population decline and removal of mature, healthy individuals Increased contaminant sources Precipitation Reduction in juvenile fitness; bioaccumulation in adults Temperature High winter flow may affect spawning habitat Change in deposition rates Permafrost thaw Increased potential for establishment of invasive macrophytes and changing fire dynamics Fire Permafrost Change Agents Drivers CE General Effect CE-Specific Effect Increase in winter habitat for juveniles Precipitation Increased contaminant sources Increased toxicity Contaminants Harvest Invasive Macrophytes Chinook Salmon Oncorhynchus tshawytscha Habitat Sedimentation of gravel-substrate will reduce quality of spawning habitat; Temporary increases in nutrient inputs could increase juvenile foraging Reduction in age at maturity; earlier spawning season; increased parasite infection Reduction in spawning and rearing habitat Human Uses Habitat loss, changes in migration routes, increased sedimentation Climate Change Direct population decline and removal of mature, healthy individuals Reduction in juvenile fitness Change in deposition rates Temperature Increase stream flow overwinter reduce egg survival Permafrost thaw Expanded ice-free season Increased potential for establishment of invasive macrophytes and changing fire dynamics Fire Mining Infrastructure Increased potential for establishment of invasive macrophytes and changing fire dynamics Invasive Macrophytes Fire Mining Precipitation Reduction in age at maturity; earlier spawning season; increased egg incubation time Chum Salmon Change Agents Drivers CE General Effect CE-Specific Effect Oncorhynchus keta Habitat Reduction in spawning habitat Habitat loss, changes in migration routes, increased sedimentation Direct population decline and removal of mature, healthy individuals Increased stream discharge could increase sedimentation and scour eggs Increase stream flow overwintr reduce quality of spawning habitat and egg survival Permafrost Infrastructure Harvest Permafrost thaw Expanded ice-free season Temperature Sedimentation of gravel-substrate in streams will reduce quality of spawning habitat Human Uses Climate Change Change Agents Drivers CE Permafrost Connected Lakes Invasive Macrophytes Infrastructure Temporary increases in nutrient inputs ; postfire landslides and debris flows Human Uses Outcompete native aquatic and emergent vegetation Climate Change Direct destruction of lake habitat Temperature Lake drying in summer decreasing connectivity; expanded ice-free season allow for early wildlife use (birds and fish); changes in thermal regimes Permafrost thaw Precipitation Decrease in lake area; lake drainage; increase in methane emissions Lake area increase through increased precipitation; increased winter habitat for aquatic species Increased potential for establishment of invasive macrophytes and changing fire dynamics Fire Mining Change Agents Drivers CE Mining Permafrost Infrastructure Disconnected Lakes Invasive Macrophytes Temporary increases in nutrient inputs; postfire landslides and debris flows Human Uses Outcompete native aquatic and emergent vegetation; faster growing vegetation overtaking lake area Climate Change Direct destruction of lake habitat Temperature Lake drying in summer decreasing lake area; expanded icefree season allow for early wildlife use (birds and fish); changes in thermal regimes Permafrost thaw Precipitation Decrease in lake area; lake drainage; increase in methane emissions Lake area increase through increased precipitation; increased winter habitat for aquatic species Increased potential for establishment of invasive macrophytes and changing fire dynamics Fire Change Agents Drivers CE Permafrost Streams Invasive Macrophytes Mining Infrastructure Temporary increases in nutrient inputs; post fire landslides and debris flows; increased channel disturbance; altered riparian vegetation and stream shade, temperature change regimes Human Uses Outcompete native aquatic and emergent vegetation Climate Change Direct destruction of stream habitat, change in conductivity, reduced flow Temperature Warming could increase extent of available habitats; lethal temperature limits for fish and other aquatic organisms ; change in thermal regimes Permafrost thaw Precipitation Increased sedimentation rates Altered hydrologies; increased channel disturbance from flooding; increased discharge and sediment transport; increase in winter precipitation will increase wildlife overwinter habitat Increased potential for establishment of invasive macrophytes and changing fire dynamics Fire Management Questions How, where, and when could Essential Fish Habitat (EFH) be affected by predicted changes in climate? - Primarily a literature review. SNAP does not currently have models predicting changes in aquatic habitats, such as stream temperature or hydrologic regime Photo: USFWS Management Questions Where and how might mineral resource development affect fishery habitat? - - From BSWI RMP: field validated information on historic and current mining sites and high, medium, and low mineral potential by sections Other options include ARDF and permit data Photo: USFWS Review Please review and provide comments: - Distribution models for fish and habitats - Conceptual models and text descriptions for fish Not yet final: - Northern pike distribution model - Conceptual models and text descriptions for habitats Contact: Rebecca Shaftel [email protected], 907-786-4965 Photo: USFWS