Friday, January 30, 2009
Thursday, January 29, 2009
paris, je t'aime!
everything is going so great - paris is absolutely as amazing and beautiful as it seems! delicious pastries & beautiful art!! tomorrow we might be going up into notre dame (it was closed today) & definitely up into the eiffel tower. but we walked all over today, through the louvre (wow!!), & just as we came upon the eiffel tower for the first time it was dusk. then the lights turned on & maybe 3 minutes later -- the most amazing light show!! the whole eiffel tower lit up & sparkling!! miss you all!
Wednesday, January 28, 2009
Tuesday, January 27, 2009
Madrid!!
We have been in Madrid for 2 days. It´s beautiful & very busy. But we´re off to Paris in the morning. We´ll get there around 2:30pm our time. Very exciting. We will be staying within miles of Versailles, Notre Dame, & of course the Eiffel Tower. We will be sure to post pictures of both Spain & Paris next time we have internet access (which is hard to come by here in Madrid!!)
love & miss you all!!
:)
Josh & Leslie
Saturday, January 24, 2009
Galway
It's wayyy colder here than in Dublin. I suppose because it's so much closer to the coast. We are definitely bundled up but we brought the right stuff so we're comfy. :) We also stayed in the Kinlay House Hostel last night. That was an experience in itself haha. But we got lucky. We booked an 8 bed room but were upgraded to a 6 bed room & THEN we didn't have anyone else in the room with us. So it was just a cheap hotel room with a community bathroom/shower down the hall. AND we had free breakfast!! So not too shabby for our first stay in a hostel. I'm sure they won't all be so wonderful... But here's hoping!
Love you guys!
Josh & Leslie
Thursday, January 22, 2009
DUBLIN!!!!
Wednesday, January 21, 2009
Dublin --
We'll write as soon as we can. Keep praying for us.
Josh & Leslie
Sunday, January 18, 2009
Wednesday, January 14, 2009
For Mike McCormick
Lake-effect snow is produced in the winter when cold winds move across long expanses of warmer lake water, providing energy and picking up water vapor which freezes and is deposited on the lee shores. The same effect over bodies of salt water is called ocean effect snow, sea effect snow, or even bay effect snow. The effect is enhanced when the moving air mass is uplifted by the orographic effect of higher elevations on the downwind shores. This uplifting can produce narrow, but very intense bands of precipitation, which deposit at a rate of many inches of snow each hour and often bringing copious snowfall totals. The areas affected by lake-effect snow are called snowbelts. This effect occurs in many locations throughout the world, but is best known in the populated areas of the Great Lakes of North America.
If the air temperature is not low enough to keep the precipitation frozen, it falls as lake-effect rain. In order for lake-effect rain or snow to form, the air moving across the lake must be significantly cooler than the surface air (which is likely to be near the temperature of the water surface). Specifically, the air temperature at the altitude where the air pressure is 850millibars (roughly 1.5 vertical kilometres) should be 13°C lower than the temperature of the air at the surface. Lake-effect occurring when the air at 850 millibars is much colder than the water surface can produce thundersnow, snow showers accompanied by lightning and thunder (due to the larger amount of energy available from the increased instability).