Cross-section map reference
Cross sections through digital terrain model of Crowberry Bog.
Cross-section map reference
Cross sections depicting elevations extracted from Lidar-derived canopy surface model. Red dots indicate local peaks and associated labels indicate the distance along the cross-section.
Cross sections depicting elevations extracted from Lidar-derived canopy surface and terrain models.
Cross-section map reference
Cross sections depicting elevations extracted from Lidar-derived canopy surface model.
Lidar-derived canopy height chartersitics for 10m buffer surrounding RRQRR sample draw.
Mean daily maximum calculated for each month of the year minus the mean daily maximum temperature for the period 1980-2010
Mean daily maximum calculated for each month of the year minus the mean daily maximum temperature for the period 1980-2010
FORKS 1 E, WA US (Station ID: GHCND:USC00452914)
Note: adjust slider to change range and hover mouse over plots to see data values.
Temperature
Precipitation
FORKS 1 E, WA US (Station ID: GHCND:USC00452914)
Just some things for context. Not worked up in any meaningful way yet…
Geological map of the Olympic Peninsula. (Source: Gavin et al. 2013. Data from Washington Division of Geology and Earth Resources staff 2008)
Cross-section map reference
“Top: Extents of late Pleistocene glacial advances in the Hoh Valley of the western Olympic Mountains (purple) and of the Cordilleran Ice Sheet in the Puget Sound (red). Dates are from Booth et al. (2003) and Thackray (2008). Bottom: The Greendland oxygen isotope record (North Greenland Ice Core Project members 2004) indicating temperature in Greenland at 50-year intervals to the last interglacial (marine oxygen isotope stage 5e). Note that the dates of the Hoh glacial advances generally date to stadial (cold) periods during stage 3 (dashed lines) and that the very extensive Lyman Rapids glacial advance falls during the cold stage 4.” (Source: Gavin et al. 2013, Figure 20)
Postglacial climate