Well, I've been on quite a tear recently as far as disabling personal electronics goes. On the morning of day 1 of my trip to Oregon, I watched as my camera bounced off of a series of lava rocks after it fell off of a sign while taking a picture. Unfortunately the fall seems to have been fatal, although I should still be able to recover the few pictures I had already taken to that point.
Then yesterday, while schlepping logs around my backyard, I totally smashed the screen on my cell phone. It still works, but i can't see what I'm doing and text messages are done for awhile. Fortunately my contract is up soon and I'm going to be switching carriers and getting some new fangle-dangle fancy phone.
**The title from this is a reference to a funny story that you don't know about. But don't worry, I'll be writing about it soon.
Thursday, August 19, 2010
Wednesday, August 18, 2010
Could today be the day?!?
It's mostly clear outside right now, with no rain reported since midnight and a forecast of partly sunny skies with patchy morning fog. Could today be the first day since July 17 with no rain? I hope so!
Thursday, August 5, 2010
Eric's big-ass ride
I'm leaving Anchorage tomorrow morning and flying down to Oregon for my friend Garry's wedding which conveniently doesn't happen until over a week later. In the meantime I'll be meeting up with my dad in Redmond and biking with him on the last few days of his cross-country ride. I kind of feel like its poor form to show up at the end of this epic journey as they cruise towards the coast, but that is outweighed by the fact that it sounds pretty cool to me that after crossing the Cascades on my first day we'll be on flats or downhills for virtually all of the remaining 175 miles or so. Also, I plan to be on hand as a photographer for all the riders once they reach the ocean, so that has to carry some value.
Anyway, it might not be too much of a ride compared to my dad's trek, but I've been looking forward to this trip for awhile and can't wait to get started.
Anyway, it might not be too much of a ride compared to my dad's trek, but I've been looking forward to this trip for awhile and can't wait to get started.
Friday, July 30, 2010
Beth's brothers were in town for a bit over a week. As predicted, several hijinks ensued. Here's the evidence:
The first stop of the trip was Homer, Alaska. Allegedly it's the halibut capital of the world, but we didn't even see one.
Well, there you have it: a photo journal which chronicles 2 or 3 of the many many more things that happened while Beth's brothers were in town. Hope you enjoyed!
Impending Vacation
There's probably other ways to define a vacation, but if you go with "missing multiple days of work to go someplace and have fun" then I'm a week from going on my first vacation since... well, since before I had a job to take a vacation from. I find that I am beginning to look forward to this thing.
Tuesday, July 27, 2010
Dew
Back when I started this thing, one of the major goals was to answer the types of questions that a person might come up with at a bar, while on a bike, or at least during a non-biking interval of a cross-country bike trip. Questions of the “the hell / anyway” variety, one of which came up recently on my dad’s blog: How the hell does dew form anyway?
Well first of all, what (the hell) is dew (anyway)? Simply put, dew is just water droplets that form on exposed objects that have cooled to temperatures below the aptly-named “dew point –“ the temperature at which the relative humidity of air would be 100%.
(The difference between dew and fog is that the water droplets in fog remain suspended in the air [while the difference between fog and mist has to do with density, where fog is the denser of the two {and the difference between mist and haze is dependent on relative humidity, with mist occurring at >95% humidity and haze under drier conditions}])
Calm weather and a lack of moisture in the upper atmosphere generally contribute to dew formation by enhancing radiative cooling at ground level. In some cases, however, where the moisture that forms dew comes from the atmosphere, a very small amount of atmospheric turbulence is needed to replenish moisture at the ground and sustain dew formation. Wet soil is also a major source of water vapor, especially since the ground can remain significantly warmer even at shallow depths than at the surface. As water vapor moves up from the warmer subsurface to the cooler surface, the dew that forms is said to be produced by distillation (yum!).
Technically speaking, it is dew that forms on cold glasses, be they of the “pint” or the “eye” varieties, when they are exposed to warm, moist air. Interestingly (but not really), pint glasses are then said to be “frosted” (a type of dew), while the more generic term “condensation” is generally used for eye glasses. Guttation – which is basically how plants pee – should probably not be confused with dew.
Well first of all, what (the hell) is dew (anyway)? Simply put, dew is just water droplets that form on exposed objects that have cooled to temperatures below the aptly-named “dew point –“ the temperature at which the relative humidity of air would be 100%.
(The difference between dew and fog is that the water droplets in fog remain suspended in the air [while the difference between fog and mist has to do with density, where fog is the denser of the two {and the difference
Calm weather and a lack of moisture in the upper atmosphere generally contribute to dew formation by enhancing radiative cooling at ground level. In some cases, however, where the moisture that forms dew comes from the atmosphere, a very small amount of atmospheric turbulence is needed to replenish moisture at the ground and sustain dew formation. Wet soil is also a major source of water vapor, especially since the ground can remain significantly warmer even at shallow depths than at the surface. As water vapor moves up from the warmer subsurface to the cooler surface, the dew that forms is said to be produced by distillation (yum!).
Technically speaking, it is dew that forms on cold glasses, be they of the “pint” or the “eye” varieties, when they are exposed to warm, moist air. Interestingly (but not really), pint glasses are then said to be “frosted” (a type of dew), while the more generic term “condensation” is generally used for eye glasses. Guttation – which is basically how plants pee – should probably not be confused with dew.
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