Moose Day Summary Report 8th Annual February 27th, 2016

Similar documents
NATURE MAPPING JACKSON HOLE.

Relationship between weather factors and survival of mule deer fawns in the Peace Region of British Columbia

Environmental. Plan Update. By Jodie Pavlica

Wyoming Pre-Workshop Survey Results August 27, 2015 Lander Wyoming

A Review of the 2007 Water Year in Colorado

Grant Opportunity Monitoring Bi-State Sage-grouse Populations in Nevada

FORECASTING FOR A HELICOPTER SKIING OPERATION IN THE UNITED STATES. High Mountain Heli-Skiing P.O. Box 2221 Jackson Hole, WY ABSTRACT

2010 Wildlife Management Unit 347 moose

2010 Wildlife Management Unit 347 moose

What Can Citizen Scientists Tell Us about Drought?

SEASONAL RESOURCE SELECTION BY INTRODUCED MOUNTAIN GOATS IN THE SOUTHWEST GREATER YELLOWSTONE AREA

2009 WMU 525 Moose. Section Authors: Nathan Carruthers and Dave Moyles

2009 WMU 349 Moose. Section Authors: Curtis Stambaugh and Nathan Webb

2010 Wildlife Management Unit 340 moose

ADMINISTRATIVE PROCEDURES

POPULATION DYNAMICS OF THE JACKSON ELK HERD

Trip and Parking Generation Study of Orem Fitness Center-Abstract

Messages of the Day November 2012

OUT OF THE DARKNESS AN ECLIPSE AND A POWER OUTAGE. Or..

2013 Snake River Fall Chinook Salmon Spawning Summary 2,667 2, ,391

Good Spirit School Division Parents/Guardians

Watershed Detectives:

Moose Stratified Block Census, Management Unit 8-5, Okanagan Region, February 2005

-Assessment of current water conditions. - Precipitation Forecast. - Recommendations for Drought Monitor

White-tailed Deer Winter Severity Index Volunteer Winter Weather Monitors Required

2010 Wildlife Management Unit 358 moose

Martin County Blizzards & Snowstorms

collision analyses...

Update on Seasonal Conditions & Summer Weather Outlook

FACETED SNOW AND DEEP SLAB INSTABILITIES IN THE MARITIME CLIMATE OF THE CASCADES. Jon Andrews* Stevens Pass Ski Area

Improving Understanding of Drought Impacts through Citizen Science

Tornadoes pose a high risk because the low atmospheric pressure, combined with high wind velocity, can:

Putative Canada Lynx (Lynx canadensis) Movements across I-70 in Colorado

Lesson Nine Population Problems. Key question How does growth of Florida s human population affect bear populations?

PAWS Science Grade 4 Released Items With Data Life Systems

PROGRESS REPORT for COOPERATIVE BOBCAT RESEARCH PROJECT. Period Covered: 1 January 31 May Prepared by

Twelve Moons Curriculum Overview

Upper Missouri River Basin February 2018 Calendar Year Runoff Forecast February 6, 2018

Highlights of the 2006 Water Year in Colorado

Satellite User Readiness through Training: VISIT, SHyMet, WMO VLab, and Liaisons

Transportation and Road Weather

Tracking the Salt Front

LOGISTICS CLUSTER SOUTH SUDAN ASSESSMENT

* Population Dynamics

Here s what a weak El Nino usually brings to the nation with temperatures:

Average Weather For Coeur d'alene, Idaho, USA

Your web browser (Safari 7) is out of date. For more security, comfort and. the best experience on this site: Update your browser Ignore

1.Introduction 2.Relocation Information 3.Tourism 4.Population & Demographics 5.Education 6.Employment & Income 7.City Fees & Taxes 8.

THE WEATHER CASE STUDIES

STATISTICAL ANALYSIS OF LAW ENFORCEMENT SURVEILLANCE IMPACT ON SAMPLE CONSTRUCTION ZONES IN MISSISSIPPI (Part 1: DESCRIPTIVE)

Upper Missouri River Basin December 2017 Calendar Year Runoff Forecast December 5, 2017

SEA LIFE Sydney Aquarium. Penguin Expedition Self-Guided Resource Kit. Secondary 7-10

NIDIS Intermountain West Drought Early Warning System December 11, 2018

Monthly Long Range Weather Commentary Issued: APRIL 1, 2015 Steven A. Root, CCM, President/CEO

106 PURDUE ENGINEERING EXTENSION DEPARTMENT

ALBERTA NATURE WINTER

Pacific Decadal Oscillation ( PDO ):

Francine s bone density is 1.45 standard deviations below the mean hip bone density for 25-year-old women of 956 grams/cm 2.

Progress on Defense-Related Uranium Mines Program

VIRGINIA S I-77 VARIABLE SPEED LIMIT SYSTEM FOR LOW VISIBILITY CONDITIONS

Field Observations and One-Dimensional Flow Modeling of Summit Creek in Mack Park, Smithfield, Utah

2014 Annual Mitigation Plan Review Meeting

Weather Outlook: 2015 Growing Season

CITY OF MINOT SNOW REMOVAL PLAN JANUARY 2015

Applications/Users for Improved S2S Forecasts

HW: Scatter Plots. 1. The scatter plot below shows the average traffic volume and average vehicle speed on a certain freeway for 50 days in 1999.

Daily Operations Briefing Friday, March 17, :30 a.m. EDT

FIGURE 1 Example schematic of flagging model. Study Design and Results

MOUNTAIN SKILLS: HOW TO REALLY READ THE AVALANCHE FORECAST

Today s Airtime: 4.6 Total PIC Time: Total Logged Time:

IMPLEMENTATION OF THE WHOOPING CRANE MONITORING PROTOCOL FALL/WINTER FINAL REPORT

SUMMARY REPORT. 11 February Deer Distance Sampling Population Estimate. Town and Country, Missouri. White Buffalo, Inc.

WRTM and Active Transportation and Demand Management

Contemporary Tectonics and Seismicity of the Teton and Southern Yellowstone Fault Systems- Phase I

Climate also has a large influence on how local ecosystems have evolved and how we interact with them.

9.1. Representing Inequalities. Explore Inequalities. Focus on

U.S. ARMY CORPS OF ENGINEERS

Lake Tahoe Watershed Model. Lessons Learned through the Model Development Process

Pierce Cedar Creek Institute GIS Development Final Report. Grand Valley State University

Office of the Washington State Climatologist

Continental Divide National Scenic Trail GIS Program

Bipole III Transmission Project Adjusted Route Assessment for Boreal Woodland Caribou and Moose

I/AA-319 Mauererberg / Munt Muro (2332 m)

Analysis of Road Sediment Accumulation to Monumental Creek using the GRAIP Method

Chippewa County Natural Hazards Mitigation Plan

COMMUNITY EMERGENCY RESPONSE TEAM TORNADOES

Bipole III Transmission Project Construction Environmental Protection Plan Construction Section N1 Environmentally Sensitive Site Locations Map 25

Snow / Inclement Weather Closure Policy

CITY OF MINOT SNOW REMOVAL PLAN November 2017

Lynx and Other Carnivore Surveys in Wisconsin in Winter

Arizona Recreation Map By Benchmark Maps READ ONLINE

Application and verification of ECMWF products 2017

4th Grade Social Studies First Nine Weeks

WWA Summer Tour. Tuesday, June 20, Lander, Wyoming. Contents. Final Water Forum for Snowcover & Stream flow Generation

SONOMA COUNTY ASTRONOMICAL SOCIETY

NEWS RELEASE. Province boosts winter highway safety measures

BISTI / DE-NA-ZIN WILDERNESS

AVALANCHE ACTIVITY ON US HIGHWAY 12. Mick Riffie Idaho Transportation Department Lowman, ID

Tornadoes. Tornadoes COMMUNITY EMERGENCY RESPONSE TEAM TORNADOES

NIDIS Intermountain West Drought Early Warning System April 18, 2017

Transcription:

Moose Day Summary Report 8th Annual February 27th, 2016 Photo taken by Kathy McCurdy. Moose Day 2016 Prepared by: Paul Hood and Alyson Courtemanch Jackson Hole Wildlife Foundation Nature Mapping Jackson Hole Program, P.O. Box 8042, Jackson, Wyoming 83002

2016 marks the eighth annual Nature Mapping Jackson Hole (NMJH) Moose Day survey conducted in collaboration with the Wyoming Game and Fish Department (WGFD). Volunteer assistance was provided by Nature Mapping Volunteer Citizen Scientists, Wyoming Game and Fish Department, Grand Teton National Park and the Bridger-Teton National Forest. The purpose of Moose Day is to educate and engage citizen scientists while recording moose observations, document moose in areas that are difficult for the WGFD to survey (mostly private lands in the more developed areas), and contribute to tracking moose population trends in Jackson Hole over time. In 2016, 61 areas of varying size were surveyed by 73 trained NMJH volunteer observers. These observers dedicated a combined total of 259 volunteer hours searching. Volunteers searched for moose by car, skis, snowmobiles and on foot. The survey areas were located between Pacific Creek and Buffalo Valley on the north end of Jackson Hole to the Hoback and Snake River Canyons to the south. Surveys were conducted between daylight (approximately 7:00 AM) and noon by car, skis, foot or snowmobile (Gros Ventre drainage). Observers used public access and vantage points, obeyed winter range closures and accessed private lands with permission. Detailed search area maps and protocols were provided to each observer. All moose observations were entered into the Nature Mapping on-line database. Only live moose were recorded while deceased moose, tracks and other sign were omitted. Ninety nine individual moose were observed in 2016 (Figure 1). Table 1. Total moose observed during Moose Day from 2009-2016. Year Date Total Moose Observed 2009 April 18 95 2010 February 27 86 2011 February 27 124 2012 February 25 94 2013 February 23 67 2014 March 1 74 2015 February 28 97 2016 February 27 99 Since 2009 s survey was conducted in April, a direct comparison is not appropriate based on different moose habitat use between February and April. Surveys in 2010-2013 and 2015-2016 were conducted in late February, and 2014 on the first day of March, thereby allowing for a comparison between years. Weather: NMJH Moose Day Report 02/29/2016 Page 2 of 6

Weather conditions were clear and cold, resulting in good visibility. The Snake River Basin was at 94% of the 30-year average of snow water equivalent as of March 1, 2016 (NRCS Snotel snow water equivalent data found at (http://www.wrds.uwyo.edu/wrds/nrcs/snowprec/snowprec.html) (Table 2). The snow water equivalent measures the depth and density of the snowpack. Higher snow water equivalents indicate a deeper, denser snowpack and lower ones indicate a shallower, less dense snowpack. In general, a deeper and denser snowpack causes moose to become more concentrated on valley bottoms and closer to roads, leading to higher observability on Moose Day. Table 2. Snow water equivalent measurements and observer visibility scores from 2010-2014. Year Date of Average Snow Water Equivalent Observer visibility 2010 n/a 55% good 2011 3/16/11 111% excellent 2012 3/29/12 88% poor 2013 3/10/13 89% poor 2014 3/10/14 142% poor 2015 3/1/15 99% good 2016 3/1/16 93% good Low snow water equivalent measurements may enable moose to disperse across the landscape while higher snow water equivalents measurements may limit dispersal, restricting moose to the valley floor. This difference in snow water equivalent between the years could in part account for the varying numbers of moose observed. Variation in visibility conditions, such as in 2014, also has a direct effect on the number of moose observed. A continuation of this project into future years and a comparison with WGFD annual population estimates may provide for better comparisons between with similar environmental conditions and an overall trend. The data from NMJH Moose Day is most appropriately used as an indicator of moose population trend over time vs. year-to-year comparisons. Survey Areas: The five survey areas added in 2011 were assessed after the 2012 count and four will be maintained into the future. The 2011 report incorrectly reported that six areas were added. One of the new areas (Emily s Pond area at the Wilson Snake River Bridge) accounted for one and two additional moose in 2011 and 2012, respectively. Survey areas were reworked slightly and renumbered for 2013. No areas with moose observations will be removed. Survey areas for 2015 were identical to the 2013 and 2014 survey areas (Figure 1). Summary: 61 individual search areas were covered by 73 volunteers 99 individual moose were observed (Figure 1) NMJH Moose Day Report 02/29/2016 Page 3 of 6

Sex and age identification are difficult in February due to antler drop in December and January. Thus, many observations are recorded as unknown (Table 3). Table 3. Moose observations in 2016 by sex and age. Sex/ Age Adult Yearling Juvenile Unknown TOTAL Female 44 0 4 0 48 Male 24 0 5 0 29 Unknown 6 1 11 4 22 TOTAL 75 0 20 4 99 Figure 1. A total of 99 individual moose were observed during the sixth annual Moose Day 2016 NMJH Moose Day Report 02/29/2016 Page 4 of 6

In 2016, 73 individual people (38 people units) spent 259 total hours volunteering for a total effort of 108 hours (73 hours by car, 8 hours by foot and 19.5 hours by skis) (Table 4). Search effort was not recorded in 2009 or 2010. Search efforts for 2011 and 2012 were calculated based on the 2012 method. A more streamlined effort calculation was used in 2012 than in the 2011 report. This 2012 method more accurately represents the volunteers effort covering the search areas rather than purely the hours volunteered. The 2012 method used people units rather than just the raw number of people. Table 4. Numbers of people, hours volunteered and search effort on Moose Day from 2009-2016. Year People People Units a Total Hours Volunteered b Total Effort c 2009 57 - - - 2010 47 - - - 2011 46 31 137.5 88.8 2012 70 49 177.3 103.5 2013 80 40 291.45 132.45 2014 71 36 240.5 115.5 2015 71 39 214 108 2016 73 38 259 100.5 a People Units represent the unit traveling together. For example, two people in one car represent one people unit and three people in one car also equate to one people unit. b Total Hours Volunteered is the sum of each team s number of people multiplied by the number of hours spent searching. c Total Effort represents the sum of each team s people units multiplied by the number of hours spent searching. The majority of volunteers worked in teams per our 2011 recommendation. This teamwork increased the number of volunteers involved and hopefully increased the observers ability to spot moose especially given the poor visibility conditions this year. Volunteers continue to be enthusiastic with regard to the Moose Day project and express their appreciation and willingness to participate in systematic, focused projects. Again, this year volunteers gathered for lunch after the counting was complete to exchange stories and report in their observation numbers. In 2014-2016, we increased our training of sex and age identification by providing a Moose ID class the week prior to Moose Day. The training s are well attended and will continue to be offered prior to future Moose Days. NMJH Moose Day Report 02/29/2016 Page 5 of 6

Recommendations: Continue to have all searching teams have a minimum of two observers, as it is often difficult to search and drive at the same time. In high snow years, the snow banks are at times higher than the vehicles thereby making a second set of observer eyes even more advantageous. Have observers document their search route and vantage points (2009 recommendation). A recommendation in 2012 was to plan a backup day in case of bad weather. This idea seems logistically very challenging and should be entered into with caution if at all. Moose Day 2017 is tentatively set for Saturday, February 25, 2016. NMJH Moose Day Report 02/29/2016 Page 6 of 6