Just got back from the annual meeting of the National Weather Association (NWA) in Louisville, KY. Unlike the American Meteorological Service, the NWA emphasizes operational meteorology, particularly for National Weather Service forecasters. So it's a different crowd and the conference presentations are much more commonly dealing with recent and historical case studies rather than purely theoretical studies.
One complete session this year was focused on the tornado and severe storm outbreak that occurred on February 5-6 of this year, during the Super Tuesday primary election. Some noteworthy talks on tools for operational meteorology included: "High Resolution, Lower Tropospheric Radar Networks: The CASA Program" by Brenda Phillips et al.; "Using Google Earth as a Situational Awareness Tool: An NWS Central Region Headquarters Example" by Brian Walawender; and "GR Level 2 Analyst" by Mike Gibson. Some other talks that I especially enjoyed were: "The Columbus Day Windstorm of 1962" (Wikipedia) by Brad Coleman; "Wintertime Mesoscale Vortices over Lake Michigan" by Sam Lashley; and "Forecasting Cold Air Damming and the Position of the Wedge Front over Northern Georgia" by Patricia Atwell et al.
Interesting poster presentations included: "Analysis of an Undular Bore over the Gulf of Mexico on March 15, 2008" by Roger Erickson; "West Texas Mesonet Proximity Observations for Wind-Driven Wildfire Starts" by Jeffrey Vitale and T. Todd Lindley; "Point Verification of Acceptable Temperature Forecasts Across the NWS Southern Region" by Bernard Meisner and Mark Fox; and "Case Study of the 3 February 2008 Valdez Bora Wind Event" by Louise Fode and James Nelson.
Friday, October 17, 2008
Thursday, October 16, 2008
Omar Va Por El Mar
After its rapid intensification over the last couple days, Hurricane Omar has skirted Puerto Rico and the Virgin Islands. Now it will continue to accelerate northeastward into the middle of the Atlantic Ocean. Winds have already decreased from a peak of 125 mph to only 70 mph.
Speaking of hurricanes, recent preoccupation with the economic crisis and presidential election has taken hurricane recovery in Texas and Louisiana out of the spotlight even faster than usual. Nevertheless, challenges still remain for many whose homes were damaged by Gustav and Ike.
Speaking of hurricanes, recent preoccupation with the economic crisis and presidential election has taken hurricane recovery in Texas and Louisiana out of the spotlight even faster than usual. Nevertheless, challenges still remain for many whose homes were damaged by Gustav and Ike.
Thursday, September 25, 2008
East Coast Storms
A low pressure area that developed along a weakening cold front has intensified substantially over the warm waters of the Gulf Stream. Although surface winds are strong enough to be a tropical storm, the system does not really appear to be "tropical", at least not at this point. Current satellite imagery reveals a structure more similar to a "subtropical storm". There is a tight circulation of cloud bands, but not continuous convection in all quadrants or concentrated near the center. It also has some characteristics of an early fall "nor'easter".

Tropical storms are primarily driven by latent heat release from an inner core of thunderstorms with a broad area of outflow above the low. This deep warm core of rising motion is related to the relatively small area of intense low pressure at the surface. In contrast to most extratropical (i.e. not tropical) cyclones, thermal wind arguments imply that the strongest winds in a tropical cyclone will be near the surface rather than near the tropopause. With the current system, the center does not appear to be very convectively unstable and it looks like it will take on a more extratropical character over the next couple days. In any case, it will bring some messy conditions along much of the Eastern Seaboard, but probably no reason for hysteria. There is also a good discussion on Jeff Masters' Wunder Blog.
Another area of interest, to the east of the Bahamas, is definitely tropical and may have some potential for development. But it's relatively unlikely to impact the United States.

Tropical storms are primarily driven by latent heat release from an inner core of thunderstorms with a broad area of outflow above the low. This deep warm core of rising motion is related to the relatively small area of intense low pressure at the surface. In contrast to most extratropical (i.e. not tropical) cyclones, thermal wind arguments imply that the strongest winds in a tropical cyclone will be near the surface rather than near the tropopause. With the current system, the center does not appear to be very convectively unstable and it looks like it will take on a more extratropical character over the next couple days. In any case, it will bring some messy conditions along much of the Eastern Seaboard, but probably no reason for hysteria. There is also a good discussion on Jeff Masters' Wunder Blog.
Another area of interest, to the east of the Bahamas, is definitely tropical and may have some potential for development. But it's relatively unlikely to impact the United States.
Monday, September 22, 2008
First Day of Fall . . . or Spring?
It was a nice first day of fall across most of the United States today. But in the Southern Hemisphere it's the first day of spring. In some of the higher elevations of South Africa that meant a surprise snow storm that has caused problems for traffic in the KwaZulu-Natal and Eastern Cape areas.
Friday, September 19, 2008
Monsoon Flooding in West Texas?
The extensive rains across northern Mexico and West Texas from the retreating North American monsoon are bringing historic flooding to the Rio Conchos and Rio Grande. As reservoirs on the Rio Conchos overflow, the downstream cities of Ojinaga (in Chihuahua, Mexico) and Presidio (in Texas) have watched flood waters breach their levees. The deaths of the U.S. and Mexican directors of the International Boundary Waters Commission and Rio Grande Council of Governments in a plane crash while surveying the flood have added to the tragedy.
Wednesday, September 17, 2008
The Long Reach of Ike
While news coverage of the devastation from Hurricane Ike has somewhat been in competition with election and financial news, and the problems are less dramatized than with Katrina, it's important to consider how broad a swath of the country has been impacted by this storm. While Hurricane Katrina effectively wiped out infrastructure from southern Louisiana to central Mississippi, the rapid movement of Ike brought major problems all the way up to the Canadian border. This is shown dramatically by the 24 hour radar-estimated precipitation through Sunday morning.

The combination of flooding and high winds have left millions of people homeless or without power as far away as western Pennsylvania! On the other side of Ike's (fourth!) landfall, the rebuilding process is challenging the residents of Grand Turk, Inagua, Haiti, eastern Cuba, and western Cuba. The wipeout of Galveston should be compared to the destruction that Grand Turk has sustained from when the hurricane was still a Category 4 on the Saffir-Simpson scale, or the misery of Gonaives, Haiti after being inundated by four tropical cyclones in a row.

The combination of flooding and high winds have left millions of people homeless or without power as far away as western Pennsylvania! On the other side of Ike's (fourth!) landfall, the rebuilding process is challenging the residents of Grand Turk, Inagua, Haiti, eastern Cuba, and western Cuba. The wipeout of Galveston should be compared to the destruction that Grand Turk has sustained from when the hurricane was still a Category 4 on the Saffir-Simpson scale, or the misery of Gonaives, Haiti after being inundated by four tropical cyclones in a row.
Monday, September 15, 2008
A Tropical Plume
The big news story lately has of course been Hurricane Ike. However there was also an interesting situation further to the west, before the landfall of Ike. From northern Mexico up into West Texas and Oklahoma, there was a persistent swath of cloud cover and rain. In spite of some analyses, this was not primarily due to interaction with a frontal zone. Instead, it was due to a plume of mid-level tropical moisture being blown northeastwards from Tropical Storm Lowell in the Pacific. In terms of winds or direct impacts, Lowell was never much of a storm. But its remote impacts through this plume of moisture were fairly significant. To some extent this pattern simply extended the influence of the North American Monsoon System further east into the Plains than usual. Because of the relatively wet ground in northern Mexico, it was feared that there could have been particularly bad flash flooding if Ike had tracked to the west over the region. The area of East Texas that was traversed by Ike was actually somewhat in need of rain, although they obviously could have done without the high winds.

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