The No. 6 seed Arizona men's basketball team (27-7, 12-6 Pac-12) will open play in the 2013 NCAA West Regional semifinal against No. 2 seed Ohio State (28-7, 13-5 Big Ten) on March 28 at the Staples Center in Los Angeles.

This is UA's 30th NCAA Tournament appearance overall (counting two vacated appearances), and the program has an official 48-26 (.649) record in its previous NCAA Tournament action. Nine of Arizona's 15 Sweet 16 appearances have come in the West Regional, and 31 of the program's 48 NCAA Tournament wins have come through the West Region.

The UA is ranked 21st in the Associated Press poll and 20th in the ESPN/USA Today Coaches' poll (as of March 18). The Wildcats are one of 11 teams nationally to have been ranked in both polls in every ranking period this season.

The Big Ten Conference postseason tournament champion Buckeyes will enter Thursday's game with a 28-7 record (13-5 Big Ten) following their March 24 78-75 win over Iowa State. As a team, Ohio State shoots 45.6 percent from the field (886-of-1,943), including 35.8 percent (215-of-600) from three-point range, while averaging 70.2 points per game.

Opponents shoot at a 39.5 percent clip and average 58.8 points per game. Two Buckeyes average in double figures, led by Deshaun Thomas' 19.7 ppg figure. Thomas also leads Ohio State with a 6.1 rebounds per game average.

Thursday's game will be the second meeting of the two schools, with Ohio State holding a 1-0 series advantage. Like this one, the previous meeting was a neutral-site game in Los Angeles, as OSU triumphed 90-47 on Dec. 29, 1971, in the opening round of the Bruin Classic. All-time, Arizona is 0-0 in series games played in Tucson, 0-0 in Columbus, Ohio, and 0-1 in neutral-site games.

Arizona has a 33-32 (.508) record against current Big Ten Conference members and is 4-4 against the league over in its last eight meetings, last facing a Big Ten opponent on Nov. 23, 2009, in what was a 65-61 loss to Wisconsin at the Maui Invitational.

This regional appearance marks the 13th time the Cats have road tripped it to California for the NCAA Tournament, and in those 13 appearances, the UA is 13-7 (.650). Two of those appearances were regionals, as the Wildcats lost the 1976 West Regional final to UCLA in Pauley Pavilion and beat Missouri in the 1994 West Regional final at the L.A. Sports Arena en route to the Final Four.

Last week, for the second game in a row, Arizona put its opponent in an early hole and never looked back in cruising to a 74-51 win over Harvard on March 23. The Cats jumped out to a 17-2 lead, forcing the Crimson to miss its first 12 shots and connecting on 58 percent of its own in the half.

Harvard's 27.6 percent shooting was the lowest for a UA opponent in NCAA Tournament play. Mark Lyons matched a career high with 27 points, Solomon Hill added a double-double and Jordin Mayes added eight key points in the second half.

By virtue of its 23-point win over Harvard, Arizona earned a berth in its 15th Sweet 16 and the seventh for the program since 2001. In that span, Arizona's seven Sweet 16 appearances rank fourth nationally, trailing only Kansas (10), Duke (10) and Michigan State (8) when it comes to playing into the tournament's second weekend.

Mark Lyons' 63-percent shooting weekend (20-of-32) in Salt Lake City was his best back-to-back effort in efficiency and production all year. He made 12 buckets Saturday against Harvard, a career high. The 25.0 ppg scoring average in the first two games of the tournament boosted his season scoring average to 15.4 ppg. He's the 37th player in school history to score 500 points in a season.

In his nine seasons as a head coach, Sean Miller has made six NCAA Tournament appearances. The Wildcat mentor has proven to be good at advancing when he gets there, as this is his fourth Sweet 16 appearance in the last six seasons.

Since 2008, Miller is one of seven coaches nationally to appear in four or more regional semifinals in that span. The list includes Tom Izzo, Michigan State; Mike Krzyzewski, Duke; and Bill Self, Kansas (5 each); and Miller, Xavier and Arizona; John Calipari, Memphis and Kentucky; Roy Williams, North Carolina; and Thad Matta, Ohio State (4 each).

UP NEXT: A win would move Arizona into the March 30 West Regional final against the Wichita State-LaSalle winner. Game time is TBA.

Long-term droughts in Southwestern North America often mean failure of both summer and winter rains, according to new tree-ring research from a University of Arizona-led team.

The finding contradicts the commonly held belief that a dry winter rainy season is generally followed by a wet monsoon season, and vice versa.

The new research shows that for the severe, multi-decadal droughts that occurred from 1539 to 2008, generally both winter and summer rains were sparse year after year.

"One of the big questions in drought studies is what prompts droughts to go on and on," said lead author Daniel Griffin, a doctoral candidate in the UA School of Geography and Development. "This gives us some indication that the monsoon and its failure is involved in drought persistence in the Southwest."

The new 470-year-long history of summer precipitation in the Southwest covers most of Arizona, western New Mexico and parts of northern Mexico.

"This is the first time researchers have used tree rings to take a closer look at the monsoon in a large and important area of the American Southwest," said Griffin, who also is an EPA STAR Research Fellow at the UA Laboratory of Tree-Ring Research.

"Monsoon droughts of the past were more severe and persistent than any of the last 100 years," he said. "These major monsoon droughts coincided with decadal winter droughts."

Those droughts had major environmental and social effects, Griffin said, pointing out that the late-16th-century megadrought caused landscape-scale vegetation changes, a 17th-century drought has been implicated in the Pueblo Revolt of 1680 and the 1882-1905 drought killed more than 50 percent of Arizona's cattle.

Co-author Connie A. Woodhouse, UA associate head and associate professor of geography and development, said, "The thing that's interesting about these droughts is that we've reconstructed the winter precipitation, but we've never known what the summers were like."

Because winter precipitation has the strongest influence on annual tree growth, previous large-scale, long-term tree-ring reconstructions of the region’s precipitation history had focused only on the winter rainy season.

"Now we see – wow – the summers were dry, too," she said. "That has a big impact."

The team's research report, "North American monsoon precipitation reconstructed from tree-ring latewood," is scheduled for publication March 11 in Geophysical Research Letters, a journal of the American Geophysical Union.

Additional UA co-authors are David M. Meko, Holly L. Faulstich, Carlos Carrillo, Ramzi Touchan, Christopher L. Castro and Steven W. Leavitt. Co-author David W. Stahle is from the University of Arkansas in Fayetteville.

The National Science Foundation, the National Oceanic and Atmospheric Administration and the U.S. Environmental Protection Agency supported the research.

"In the Southwest, the winter precipitation is really important for water supply. This is the water that replenishes reservoirs and soil moisture," Woodhouse said. "But the monsoon mediates the demand for water in the summer."

Until recently, most tree-ring researchers, known as dendrochronologists, have looked at the total width of trees’ annual rings to reconstruct past climate. Few teased out the seasonal climate signal recorded in the narrow part of the growth ring laid down in late summer known as latewood.

To figure out the region’s past history of monsoon precipitation, the scientists needed to measure latewood from tree-ring samples stored in the archives of the UA Laboratory of Tree-Ring Research and go into the field to take additional samples of tree rings.

The team looked at annual growth rings from two different species, Douglas-fir (Pseudotsuga menziesii) and ponderosa pine (Pinus ponderosa) throughout the weather forecast region called North American Monsoon Region 2, or NAM2.

In all, the researchers used samples from 50 to 100 trees at each of 53 different sites throughout southwestern North America. The team’s climate analyses focused on NAM2, which covers most of Arizona, western New Mexico and northern parts of the Mexican states of Sonora and Chihuahua.

Griffin said, "It was a massive undertaking – we employed about 15 undergraduates over a four-year period to measure almost 1 million tree rings."

The results surprised him because rain gauge records for the Southwest from 1950-2000 show dry seasons alternated with wet ones.

However, the team's new multi-century record going back to 1539 shows that the wet/dry pattern of the latter part of the 20th century is not the norm – either prior to the 20th century or now, he said.

One possible next step, Woodhouse said, is to expand the current project to other areas of the Southwest and into Mexico, where the monsoon has a bigger influence on annual precipitation.

Another would be using tree-ring reconstructions of the Southwest’s fire histories to see how wildfires are related to summer precipitation.

Griffin said, "Before I moved to the Southwest, I didn’t realize how critically important the summer rains are to the ecosystems here. The summer monsoon rains have allowed humans to survive in the Southwest for at least 4,000 years."