1-20 OF 28 RESULTS FOR

SNOTEL

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
×Close Modal
Sort by
Series: GSA Field Guide
Published: 01 January 2009
DOI: 10.1130/2009.fld015(22)
EISBN: 9780813756158
... The field trip is a one-day loop beginning in Portland, driving east and stopping at a SNOTEL site south of Mount Hood. The trip ultimately encircles Mount Hood as it continues east of the mountain, stopping at a debris flow and on to the Columbia River and back to Portland. Abstract...
Image
Data from the Brooklyn Lake <b>SNOTEL</b> station ( USDA, 2015 ) for the 2013–2014...
in > Geophysics
Published: 29 January 2016
Figure 2. Data from the Brooklyn Lake SNOTEL station ( USDA, 2015 ) for the 2013–2014 water year, showing (a) SWE, (b) snow depth, (c) snow density, and (d) air temperature. Day 0 is 1 October 2013. Gray circle and square highlight the dates of GPR acquisition, 2 March 2014, and 27 March 2014
Image
Maps of the western USA show <b>SNOTEL</b> data for seasonal fractions of total an...
Published: 01 July 2009
Figure 4. Maps of the western USA show SNOTEL data for seasonal fractions of total annual precipitation for (A) Winter (November to March); (B) Spring (May and June); (C) Summer (July and August).
Image
Data on snow and water-equivalent precipitation, 1980-98, from <b>Snotel</b> stati...
Published: 01 May 2000
Table 4B Data on snow and water-equivalent precipitation, 1980-98, from Snotel station above head of Indian Canyon, at 39° 54′N, 110° 45′W; elevation 2775.5 m
Image
Histograms of SWE from the three lines analyzed in this paper. The mean SWE...
in > Geophysics
Published: 29 January 2016
Figure 11. Histograms of SWE from the three lines analyzed in this paper. The mean SWE on the lines is 0.61 m, slightly less than the SWE measured at the nearby Brooklyn Lake SNOTEL site on the dates of GPR acquisition (Figure  2 ). Histogram bin widths are 0.008 m in A, C, and D, and 0.006 m
Image
A: Calcite δ 18 O (reversed scale) with break indicated at A.D. 1953, when ...
in > Geology
Published: 01 March 2011
Figure 3. A: Calcite δ 18 O (reversed scale) with break indicated at A.D. 1953, when Bison Lake was impounded (1σ age model errors). VPDB—Vienna Peedee belemnite. B: White River natural flow near Watson, Utah (obtained from U.S. Bureau of Reclamation) and Bison Lake SNOTEL (snowpack telemetry
Image
A map of the western USA shows sampled lakes as diamonds and SNOwpack TELem...
Published: 01 July 2009
Figure 2. A map of the western USA shows sampled lakes as diamonds and SNOwpack TELemetry (SNOTEL) stations as squares. Sampling regions are circled: 1—Cimarron Range, 2—Canjilon and Burned Mountains, 3—San Juan Mountains, 4—Sawatch Range, 5—Front Range, 6—Park Range and Medicine Bow Mountains, 7
Image
The overview of the T.W. Daniel Experimental Forest (TWDEF) study site in n...
Published: 01 December 2014
) soil moisture sensors are shown as triangles around each plot weather station. Utah State University’s Doc Daniel SNOTEL site (USUSNOTEL) is located at the eastern edge of the TWDEF enclosure. The clay content (%) distribution inside the TWDEF site is displayed in the upper right corner. Note
Journal Article
Journal: GSA Bulletin
Published: 01 July 2009
GSA Bulletin (2009) 121 (7-8): 1179-1189.
...Figure 4. Maps of the western USA show SNOTEL data for seasonal fractions of total annual precipitation for (A) Winter (November to March); (B) Spring (May and June); (C) Summer (July and August). ...
FIGURES | View All (10)
Journal Article
Journal: Geophysics
Published: 29 January 2016
Geophysics (2016) 81 (1): WA183-WA193.
...Figure 2. Data from the Brooklyn Lake SNOTEL station ( USDA, 2015 ) for the 2013–2014 water year, showing (a) SWE, (b) snow depth, (c) snow density, and (d) air temperature. Day 0 is 1 October 2013. Gray circle and square highlight the dates of GPR acquisition, 2 March 2014, and 27 March 2014...
FIGURES | View All (11)
Journal Article
Published: 01 August 2013
Vadose Zone Journal (2013) 12 (3): vzj2012.0097.
... (25), TS (25), TA (2), P, SD (1), SWE (1) active – SMOSMANIA 21 SM (4) active ( Albergel et al., 2008 ; Calvet et al., 2008 ) SNOTEL 381 SM (16), TS, TA, P, SWEQ, SD active – SWEX_POLAND 6 SM (8), TS (13) active ( Marczewski et al., 2010 ) UDC_SMOS 11 SM (5) closed...
FIGURES | View All (15)
Journal Article
Journal: Geology
Published: 01 March 2011
Geology (2011) 39 (3): 211-214.
...Figure 3. A: Calcite δ 18 O (reversed scale) with break indicated at A.D. 1953, when Bison Lake was impounded (1σ age model errors). VPDB—Vienna Peedee belemnite. B: White River natural flow near Watson, Utah (obtained from U.S. Bureau of Reclamation) and Bison Lake SNOTEL (snowpack telemetry...
FIGURES | View All (5)
Journal Article
Journal: GSA Bulletin
Published: 01 March 2017
GSA Bulletin (2017) 129 (3-4): 500-512.
... observed shallow discharge in both the bedrock gorges and alluvial reaches, which, given that the snowpack of 2007–2008 was not exceptional ( SNOTEL, 2016 ), we infer occurs on an approximately annual basis. Though snowmelt discharge here appears minor, past work in glacial landscapes shows that meltwater...
FIGURES
Journal Article
Published: 01 May 2013
Vadose Zone Journal (2013) 12 (2): vzj2012.0170.
... ThetaProbe ML2X 0.05–0.30 4 SNOTEL 374 Hydraprobe Analog (2.5 Volt) 0.00–1.02 16 Hydraprobe Analog (5.0 Volt) Hydraprobe Digital Sdi-12 (2.5 Volt)NS SWEX_POLAND 6 D-LOG-mpts 0.00–1.00 10 PR2- Profile Probe UDC_SMOS 11 EC-ET 0.00–0.40 5 EC5 IMKO TDR...
FIGURES | View All (10)
Journal Article
Journal: Lithosphere
Published: 12 December 2018
Lithosphere (2019) 11 (1): 59-72.
... focus on n = 2/3 for all transient profile simulations. The modern relationship of elevation to “fraction of shielded cosmic rays” (F) was determined from snow water equivalency data from four nearby SNOTEL sites (Banner Summit, Bear Basin, Secesh Summit, and Long Valley) in the Salmon Basin...
FIGURES | View All (9)
Journal Article
Published: 01 January 2014
Rocky Mountain Geology (2014) 49 (1): 51-60.
... precipitation and associated dynamics, precipitation data from Colorado Climate Division 1 provide a direct representation of wet and dry cases rather than derivatives of precipitation like the Palmer Drought Severity Index (which is biased to low-elevation agricultural regions) or SNOTEL (short for SNOwpack...
FIGURES | View All (4)
Journal Article
Journal: Geology
Published: 01 December 2001
Geology (2001) 29 (12): 1095-1098.
... shielding by surrounding topography largely eliminates the need for a correction. Annual snow cover is low at the field localities, as indicated by the available record of snow course data from nearby SNOTEL stations at similar elevations (average daily water- equivalent snow cover is <7 cm...
FIGURES
Journal Article
Journal: GSA Bulletin
Published: 29 August 2017
GSA Bulletin (2018) 130 (1-2): 175-192.
... for the cave site; however, data collected since 1978 at the Mill Creek Summit SNOTEL (Snowpack Telemetry) station at a slightly higher elevation (2680 m) in the Salmon River Mountains NW of the Lost River Range are likely similar. The mean annual air temperature at the Mill Creek Summit SNOTEL is 1.1 °C...
FIGURES | View All (12)
Series: GSA Field Guide
Published: 01 January 2009
DOI: 10.1130/2009.fld015(15)
EISBN: 9780813756158
... Snotel site (Latitude: 42.71, Longitude: -118.63; elevation 2335 m) are available since the start of water year (WY) 1979. The 30-year average precipitation for this site is 117 cm falling mostly between November and May. The eastern face of Steens Mountain was carved by glaciers. In these small...
Journal Article
Published: 01 May 2000
Journal of Sedimentary Research (2000) 70 (3): 461-469.
...Table 4B Data on snow and water-equivalent precipitation, 1980-98, from Snotel station above head of Indian Canyon, at 39° 54′N, 110° 45′W; elevation 2775.5 m ...
FIGURES | View All (5)