The SJER vegetation community is mostly blue oak (Quercus douglasii), interior live oak (Quercus wislizeni), gray pine (Pinus sabiniana), California Buckeye (Aesculus californica), poison oak (Toxicodendron diversilobum) and many species of naturalized annual grasses and native grasses and forbs. Elevation of the tower is 405 m. Mean minimum T is 9.3ºC, mean maximum temperature is 23.5ºC. Mean annual precipitation is 513 mm year-1. (information from Goulden et al., 2012).
Panorama of San Joaquin Experimental Range. May 2014.
A full size image is available at the digital library.
For additional information, see Goulden et al., 2012.
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Flux Tower Transect, SJER - Flux Tower, Meteorology (2009-2016)
7 components • 405 m Flux Tower, San Joaquin Experimental Range • Biology / Ecology, Climatology / Meteorology • Mike Goulden, Anne Kelly
An eddy covariance flux tower is located near the top of the P301 watershed. Instruments collect data on temperature, relative humidity, and fluxes of carbon dioxide and water vapor to determine the physiological responses of the site (for example, how photosynthesis increases with light) and summed over a year to determine the carbon balance of a site (how much carbon it is gaining or losing). Three other flux towers have been instrumented at different elevations with the Sierras including the San Joaquin River, Soaproot, and Short Hair Creek.
This west-east transect spans elevation gradient from 400 m to 2700 m. The change in elevation is accompanied by a slight increase in precipitation, but the main change is a shift from rain-dominated precipitation to snow-dominated precipitation. The climatic shift plays out in other ways as well. At lower elevations, high temperatures and low water availability limit evapotranspiration by vegetation. Meanwhile, forest activity (evapotranspiration) at higher elevations is limited by cold winter temperatures. There is a sweet spot at middle elevations of yera-round evapotranspiration and forest activity.
This gallery showcases the landscape, vegetation, equipment and facilities at the SJER field area.
SJER – 400 m elevation
Quad: Millerton Lake
Ward Mountain Trondhjemite (Kw) (formerly Leucotonalite of Ward Mountain)
“Medium- to fine-grained biotite leucotonalite (trondhjemite). Rock appears gneissic in outcrop and deformed and recrystallized in thin section... Biotite, generally in tiny plates, is the sole primary mafic mineral. Secondary muscovite in plates as much as 2 mm across is abundant locally... U-Pb age of … 115 m.y” (Bateman and Busacca 1982). “Biotite averages about 10 percent of the rock… most samples contain less than 5 percent alkali feldspar… Deformed trondhjemite, which constitutes the bulk of the rock, is fine grained and gneissic, and when viewed in thin section it can be seen to have a granoblastic texture… The Ward Mountain Trondhjemite intrudes the Bass Lake Tonalite” (Bateman 1992).
For more detail on the other flux towers, refer to each page:
Soaproot Saddle, 1100 m elevation
Quad: Shaver Lake
Bass Lake Tonalite (Kbl, formerly Tonalite of Blue Canyon)
P301, 2000 m elevation
Quad: Huntington Lake
Dinkey Creek Granodiorite (Kdc, formerly Granodiorite of Dinkey Creek)
Short Hair Creek, 2700 m elevation
Quad: Blackcap Mountain
Aplite and felsic quartz monzonite dikes (Kap)
Granodiorite of Dinkey Creek (Kdc, see description for P301)