El Niño to make the mountains colder and drier this winter

Predicting climate in the old days relied upon observing cues in nature. The Farmers’ Almanac finds that people looked at woolly worms in late summer in get a sense of winter. The more black hairs on the worm, the colder and wetter the winter. Of course woolly worms come in all configurations of black and orange colorings so how could a worm’s coat predict winter? It can as an analogy;  you look at the forecast to decide which coat you’re going to wear before leaving home. I think you would want to wear a black coat as opposed to a white coat on a very cold and sunny day to maximize the amount of solar energy you could absorb. Woolly worms just plan far ahead.

Today we track global changes in wind patterns and sea surface temperatures to predict weather conditions. NOAA’s Climate Prediction Center has issued a climate forecast for this winter based on the El Niño pattern emerging in the Pacific Ocean.

Below are winter predictions for the U.S. indicating greater or lesser chances for departures in average winter temperatures and precipitation.

temps

precip

El Niño is a departure from average sea surface temperatures created by a change in the intensity and direction of equatorial winds. In a normal period, strong easterly trade winds blow across the Pacific and upwell cold, nutrient rich waters on the west coast of South America. These same winds also pile up water in the western Pacific so that the sea surface is about 2 feet higher at Indonesia than at Ecuador.

Normal Sea Surface Temperatures in °C

In an El Niño cycle, the winds are not as intense and warmer sea surface temperatures extend further to east. This change has a global impact on weather with increased precipitation on the west coast of South America and the south & east coasts of North America. Warmer than normal conditions also occur at higher latitudes in North America and over the Pacific ocean.

El Niño Sea Surface Temperatures in °C

El Niño Sea Surface Temperatures in °C

First freezing night in the Great Smokies

Overnight the temperature dropped to 25° F at the Newfound Gap weather station, elevation 5,000 ft. Mt LeConte at 6400 ft above sea level recorded a low temperature of 31° F.  The slight warming at 1,400 ft higher in elevation is caused by a temperature inversion that most frequently happens in autumn mornings.

The lowest temperature recored at Mt. LeConte for September 29 was 24° F and that happened in 2003. The coldest night ever recorded since 1988 was -22° F, which occurred last February 4.

Station reports for 7:30 am, September 28 – 7:30 am, September 29:

STATION             ELEV    HIGH    LOW     PCPN    SNOW DEPTH
SUGARLAND CENTER    1600     75      45     0.00
NEWFOUND GAP        5000     62      25     0.00
CADES COVE          1900     73      44     0.00
OCONALUFTEE         2040     79      42     0.00
MOUNT LECONTE       6400     57      31     0.01

http://www.outrageGIS.com/weather/grsm

All weather cams are up

Look Rock, Sept. 24

Look Rock, Sept. 24

After a few months of intermittent outage, all four weather observation cameras for the Great Smoky Mountains National Park are now operational. We archive full-day animations for 3 webcams and the visible satellite view of the park every day at:
http://www.outragegis.com/weather/img/animation/yesterday
.

For previous days, you can access other days by replacing “yesterday” with the 6-digit year month day combination. For example, for September 24, 2009 replace “yesterday” with “090924”and create this link:
http://www.outragegis.com/weather/img/animation/090924.

For highest resolution images, just click on the preview images.

The two National Park cameras are located on Look Rock and Purchase Knob. Look Rock camera overlooks most of the park. The two National Forest cameras, Cold Mountain and Joyce Kilmer Wilderness, overlook small portions of the park.

Now let’s watch fall pass in the mountains!

Sept 12: Sheltowee Trace Meeting in Winchester

The Future of the Trace: Sept 12, 2009

Join a group of trail enthusiasts and forest & park officials at the Daniel Boone NFS headquarters in Winchester to discuss the future of the Sheltowee Trace. We need as many committed folks as possible to attend. Voice your support for the Sheltowee Trace.

If you would like to attend, you can RSVP here with a comment so we can plan for breakfast and lunch!

Time: 9:30am
Where: Clark County Extension Office (map below)
1400 Fortune Dr
Winchester, KY 40391-8292
(859) 744-4682

Preliminary Agenda

9:30 to 10:00 – Meet and Greet – Coffee, Juice and Bagels, Donuts provided.

10:00 Opening Comments

  • Frank Beum, Forest Supervisor, Daniel Boone National Forest
  • Steve Handley, Big South Fork National Recreational Area, National Park Service
  • Carey Tichenor, Ky State Parks and Recreation
  • Steve Barbour, Interim Executive Director, The Sheltowee Trace Association

10:30 – Updates on the Current Condition of The Trace in each Ranger District and Plans for the next 12 to 24 months

10:45 – Current Management Plan Development

  • Federal and State Funding Levels
  • Challenges of a Muti-use Trail
  • Current on-going volunteer programs
  • Short Term and Long Term Maintenance Issues
  • Trace Blazing – Signage
  • Land Acquisition
  • Trace Relocation
  • Maintaining Easements
  • Development of the Volunteer Base
  • Promoting The Trace across the state

Following these discussion will be a session on forming the Sheltowee Trace Association, a non-profit dedicated to promoting and protecting this National Recreation Trail.

Map:Here

Woodland Art Fair, Aug 15-16

Come down to the Woodland Art Fair the is Saturday and Sunday and check out our new maps. We will have the spring release of the Red River Gorge and the Sheltowee Trace South, both of which were designed and printed in the past 6 months. The map to out booth is provided below: [Read more…]

Sheltowee Trace Suspension Bridge Quiz

How many scenic suspension bridges exist on the Sheltowee Trace and where are they? If you think you know the answer, then please take our quiz and you might win some free maps.

Directions: If you can name or locate all of the suspension bridges on the Sheltowee Trace, then you can receive our new Sheltowee Trace map for free. Name all of the them and tell us which is the largest and which is the smallest, then you’ll get three free maps of your choice.

How to submit you answer: Email your answer to contest@outrageGIS.com beginning Friday, August 21, 2:00pm EST. You must be the seventh correct email to win. You only get one try and we’ll take your first answer.

If you’re not the 7th person to answer either question correctly, then you will still receive a bonus coupon to use at our online store. Just give it a try!

Ok….which bridge is this? If you need a little help, visit http://www.sheltoweetrace.com

Lexington Community Gardens


London Ferrell Community Garden

Locations of Lexington’s community gardens. Gardens maintained by Seedleaf: Nourishing communities by growing, cooking, sharing, and recycling food.

[Read more…]

Animations of the Atmosphere

As a lover of the atmosphere and sun, I want to see how light and sky change over the course of the day. I also want to see how large-area weather events, such as the passage of a front, impact different places in the Great Smoky mountains. The inspiration behind this page was a desire to record weather changes at different elevations on a mountain and to help the photographer in me better understand a secretive and dynamic landscape.

Enter Yesterday: a site of prior-day animations of federal web cams and satellite imagery located here at http://www.outragegis.com/weather/img/animation/yesterday. Note this page always shows conditions for the prior day since they are full-day timelines.

The Great Smokies have about one mile of vertical relief and weather conditions can be dramatically different depending on your elevation. Whatever it’s a line of thunderstorms or fog in the valleys on a calm morning, this is a visual record of evolving conditions…only of course it happens during daylight. For the weather nut who likes to take it a step further, the page gives data from park’s 5 weather stations for the same day….and it’s all archived.

How was it done? After tinkering with ImageMagick and FFmpeg, I made a script that creates full-day animations of the webcams in the Great Smokies and visible satellite images from NOAA. What will it become? Consider it a visual archive of the atmosphere and movements of the Sun in the Great Smokies. Any suggestions are welcome.

Some notes for updates: I haven’t fully utilized the flash embedded video (see the two samples below, top is animated gif and below is embedded flash video). The problem is setting animations in sync together, e.g., sun rises at the same time in all movies. With an animated .gif, I think you simply need to refresh your browser after all of the images are loaded to get a partial sync. A better solution is out there. I can also increase the sampling rate for smoother play; now it’s two samples an hour.

Weather map and webcam animation for the Great Smoky Mountains

Weather map and webcam animation for the Great Smokies


[flv:http://www.outragegis.com/weather/img/animation/090603/PurchaseKnob.flv 400 290]

These are also archived, so if you go to the smokies for a backcountry trip, you’ll be able to find your days here.

Bike Lexington Month

So the month of May is nearly done and with it, ends the month-long celebration of the bike and human-powered travel. As a hiker, I often worry about my environmental impact during a drive to a favorite trailhead.

How can I minimize fuel consumption and make better? I reason that if I bike as my primary form of transportation, I will only need to drive during my trips to the woods. This works great if I have a network of safe and continuous bike lanes and trails in the city. Enter Bike Lexington.

I’m proud to say that I contributed a small share to bike community here. I took the artwork designed by Cricket Press (shown by the poster design left) and made the Bike Lexington interactive calendar (shown here), which hopefully encourages people to bike more. Building the site definitely exposed me to vibrant groups and events that helped me stay committed to biking in Lexington.

After this month is over though, biking doesn’t stop. Check out the website for new events throughout the year or join the newsletter subscription to stay updated.

Rainy May: on track to be the wettest May ever

Spring is typically a wet month. However over the past week, Eastern Kentucky has experienced unusual rainfall amounts. The record for the month is 10.78 inches in 2004; and no other year has been above 10 inches for May. The only year that saw over 9 inches of rainfall for May was in 1995. May during 1983 and 1984 were the only times over 7 inches of rainfall.

From the National Weather Service in Jackson, Kentucky:

"2 TO 5 INCHES OF RAIN HAS FALLEN ACROSS EASTERN KENTUCKY DURING THE
MONTH OF MAY. THIS IS OF INTEREST...SINCE WE ARE ONLY ABOUT ONE
QUARTER OF THE WAY THROUGH THE MONTH. HEAVY RAINFALL IS VERY
POSSIBLE AS WE HEAD INTO MOTHERS DAY WEEKEND AND COULD PUSH RAINFALL
AMOUNTS UP ANOTHER INCH OR TWO.

THE AVERAGE PRECIPITATION FOR THE MONTH OF MAY AT THE JACKSON
WEATHER OFFICE IS 4.92 INCHES. WE HAVE ALL READY RECORDED 4.12
INCHES OF RAINFALL AS OF THIS MORNING AT 7AM. IT IS TOO EARLY TO TELL
...BUT WE ARE CERTAINLY ON TRACK TO HAVE ONE OF THE RAINIEST MAYS
EVER. THE RAINIEST MAY OCCURRED IN 2004 WHEN THE JACKSON WEATHER
OFFICE RECORDED 10.78 INCHES FOR THE MONTH. THIS WAS THE ONLY MONTH
OF MAY THAT OVER TEN INCHES OF RAIN FELL. MAY OF 1995 HAD 9.91
INCHES AND WAS THE ONLY MONTH WITH OVER 9 INCHES RECORDED. THE NEXT
HIGHEST TOTALS WERE OVER 7 INCHES AND THAT OCCURRED IN ONLY TWO
YEARS...1983 AND 1984.

HERE ARE RAINFALL TOTALS FROM EASTERN KENTUCKY COOPERATIVE WEATHER
STATIONS AND AUTOMATED SURFACE OBSERVING SYSTEMS AS OF 7 AM
EDT...FOR THE MONTH OF MAY 2009.

LOCATION         /   COUNTY     /     PRECIPITATION

BARBOURVILLE         KNOX              4.38  INCHES
BAXTER               HARLAN            3.85  INCHES
BEATTYVILLE 4N       LEE               3.68  INCHES
BIG SHELBY           PIKE              3.01  INCHES
BOONEVILLE 1SE       OWSLEY            4.49  INCHES
BUCKHORN LAKE        PERRY             2.80  INCHES
CARR CREEK LAKE      KNOTT             2.73  INCHES
CAVE RUN LAKE        ROWAN             2.28  INCHES
CLAY CITY 1WNW       POWELL            2.77  INCHES
CLOSPLINT 4ESE       HARLAN            4.55  INCHES
COLO                 PULASKI           3.98  INCHES
CRESSY               ESTILL            2.59  INCHES
DRAFFIN              PIKE              3.54  INCHES
EZEL                 MORGAN            3.31  INCHES
GIMLET               ELLIOTT           2.60  INCHES
HARLAN 1S            HARLAN            3.80  INCHES
HARLAN STATE POLICE  HARLAN            2.95  INCHES
HAZARD WATER         PERRY             3.71  INCHES
HAZARD               PERRY             3.70  INCHES
HAZARD STATE POLICE  PERRY             2.95  INCHES
HEIDELBERG 2N        LEE               4.05  INCHES
BAXTER               HARLAN            3.85  INCHES
INEZ 2E              MARTIN            3.78  INCHES
ISLAND CITY          OWSLEY            5.16  INCHES
IVEL                 FLOYD             2.27  INCHES
NWS JACKSON          BREATHITT         4.12  INCHES
JEREMIAH 1S          LETCHER           3.11  INCHES
KINGDOM COME ST PARK HARLAN            3.12  INCHES
LONDON CORBIN APT    LAUREL            4.46  INCHES
MONTICELLO 3NE       WAYNE             4.00  INCHES
MOUNT STERLING 5N    MONTGOMERY        2.41  INCHES
MOUNT VERNON         ROCKCASTLE        2.77  INCHES
ONEIDA               CLAY              4.54  INCHES
PAINTSVILLE 1E       JOHNSON           3.55  INCHES
PIKEVILLE ST POLICE  PIKE              2.05  INCHES
PRESTONSBURG 3NW     FLOYD             4.09  INCHES
QUICKSAND            BREATHITT         3.52  INCHES
RELIEF               MORGAN            3.18  INCHES
ROGERS               WOLFE             2.82  INCHES
SALYERSVILLE         MAGOFFIN          4.28  INCHES
SANDY HOOK           ELLIOTT           2.67  INCHES
SKYLINE              LETCHER           3.20  INCHES
SLADE 5NE            POWELL            2.86  INCHES
SOMERSET 2N          PULASKI           3.74  INCHES
STANTON 2W           POWELL            2.88  INCHES
STEARNS 2S           MCCREARY          5.09  INCHES
VICTORY 5NW          LAUREL            4.13  INCHES
WEST LIBERTY 3NW     MORGAN            2.67  INCHES
WEST LIBERTY 11NW    MORGAN            2.57  INCHES
WHITESBURG           LETCHER           2.50  INCHES
WHITESBURG 2SE       LETCHER           3.21  INCHES
WILLIAMSBURG 1NW     WHITLEY           5.14  INCHES

THE NATIONAL WEATHER SERVICE AT JACKSON WOULD LIKE TO THANK ALL THE
DEDICATED COOPERATIVE WEATHER OBSERVERS FOR THEIR TIMELY REPORTS."

It is all about Light: a photographers dream

The past day’s weather has included periods intense light and shadow from very low, broken stratus & cumulus clouds. Rays of love from god shine from heaven through parted clouds; and there was plenty of love in the mountains. Even in these low quality webcam images, you can see golden rays of light and clearly defined ridges. Now what if you were there with a serious camera.

Though the weather overall has been chilly and uncomfortable, it does give some memorable vistas. The more diffuse stratus clouds in the western mountains were lower in altitude and created softer light.

Moon Rise
View from Purchase Knob

(raw) 3D map of Eastern Kentucky

As we gear up for the Sheltowee Trace topographic map, I thought it would be interesting to see if a complete 3d map of the ST could be printed. Unfortunately, it would have to be a huge sheet of paper to get the detail necessary for a good map. But as an online viewer, I see potential. This sample is a raw render output and you can see well the basic physiography. Now we just need to add trails, transportation, labels, etc….nothing too much, just about 6,000 sq. mi. for the Daniel Boone NF.

3D map
Explore this map through a zoomable flash map

New Red River Gorge Map

5th Edition Red River Gorge5th Edition Red River Gorge Backpacking Map

It’s almost ready for release!
A complete remake of our popular backpacking guide with the green maps. This new set keeps all of the great features of the old maps, but in full-color and updated trails and data.

Visit our Gorge webpage to learn more: http://www.outrageGIS.com/gorge

In January we looked at the previous editions, all 2-color with an travel elevation profile booklet, and thought how we could improve it. We had used aerial photography to show landcover type, which did a good job indicating density of canopy, open areas, sunlight, and offered a rustic green background for our GPS trails.

However, most people are confused when they look at aerial photographs…they think hills are valleys and vice versa. This terrain inversion is a significant cartographic problem, but we were confident then when most people *used them in the field* they made sense.

While unique advantages exist using photographs, for the new edition we used a custom created, full-color hillshade that shows forest canopy cover type and open areas. We artificially lit the landscape from the west and eliminated terrain inversion. We added a distinct stream symbol to clearly mark drainage. With 50-foot contours and spot elevations, this new edition offers a handsome way to stay located.Gray's Arch rockshelter

Since most GPS applications are now by default in the latitude/longitude (decimal degrees) coordinate system, we added this graticule to the map. A UTM grid is also labeled. With scales on the corners of maps that can be seen while folded, a hiker can quickly determine distance and locate themselves with a GPS in either dd.dddd or UTM coordinate systems.

We still have all of the trail profiles, side trails, backcountry campsites that were in the previous edition. The new edition actually covers more area and trails.

Red River Gorge Backpacking Map: $14

A Tale of Two Smokies

Visible Sat April 15, 2009. We see two very different Smokies today and the highest peaks in the southern Appalachians provide an atmospheric boundary.

On the west side of the mountains we see low dense stratus clouds, but on the east side we have clear skies. As the atmosphere is uplifted over the the highest ridge of mountains there’s cooling and abundant cloud formation. That’s half the story.

The winds are form the northwest and the Smokies (along the Tennessee/North Carolina stateline) provide the highest barrier the winds must cross over. On the leeward side, as the winds cross over the mountains, they descend, warm, and prevent cloud formation especially just east of the summits.

Link to more: http://pixel.outragegis.com/v/weather_maps/090415_TwoSmokies/
These images and animation show a textbook situation of topographic control of weather, but over a very large area.

  

Why we use aerial photography

Many customers ask us why we use aerial photography. Often it’s hard for some readers to understand because of terrain inversion. Let’s take a Q&A with a real customer:

Customer, “Hi guys. I just wonder if anyone has ever discussed with you the fact that the shading on your maps appears to be reversed. That is, the high points appear like low points and vice versa, if one is looking at the map oriented to north. If one turns the map around, so it is oriented to south, then everything looks correct. So, my guess is simply that the shading is on the wrong side of the ridges. ”

Our response, “Thanks for asking a question that has popped up a few times. In the mapping biz, it’s called terrain inversion and it is a problem sustained by tradition. Before aerial photography, most terrains were shaded as if the sun was in the upper-left corner. This was established as cartographic tradition because we read from upper-left to lower-right.

This worked fine until aerial photography became used as base maps. In the northern hemisphere, and especially at our latitude, the sun is never shines from the north. All of our shadows fall from south to north, completely opposite to how they’re depicted on most conventional maps. Cartographers in the southern hemisphere think we’re crazy up here moving the sun around to accommodate tradition at expense of reality. But they have the advantage of sun always being in the upper quadrants, thus giving the type of illumination you’re probably used to.

But we use aerial photography in most of our maps, because it is reality and at the right scale is far superior to an artificial hillshade in our opinion for couple reasons. You can see areas that are really in shadow, which indicate different plant communities. You can see canopy type, density, and other indicators for type of forest. If you’re a photographer, these images show depth and lines of shadow, helping you predict the kind of light you want for a photo. Finally, if you have take an aerial photo up high to orient, you can do so by shadows.

Detail from our Big South Fork map with aerial photography. Note the north facing cliffs are in shadow, just as in found in the wild.

So in my defense, I say it’s all about sunlight. I understand your problems and trust me, it has stirred the anger of my peers at cartography conferences. We’ve been flamed on blogs for this apparent flaw, but in our humble opinion, an aerial photo is not the problem, it’s tradition.

It’s sounds like you have a lot of experience with maps, and I respect your opinion. However, I think if you get used to aerial photography, you’ll find distinct advantages. Also in defense of tradition, I did illuminate our recent map, Trail Atlas of the Great Smokies from the NW. That map does not use aerial photography so it was an easy decision.”

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