Search by property

Jump to: navigation, search

This page provides a simple browsing interface for finding entities described by a property and a named value. Other available search interfaces include the page property search, and the ask query builder.

Search by property

A list of all pages that have property "QCnotes" with value "3-year smoothed". Since there have been only a few results, also nearby values are displayed.

Showing below up to 49 results starting with #1.

View (previous 50 | next 50) (20 | 50 | 100 | 250 | 500)

    

List of results

    • SAm 032.temperature  + (7-year filtered. Errors are given as the confidence intervals; correlation with 4- year lag)
    • Arc 045.temperature  + (A newer, higher-resolution record has been published by Jiang et al. (2015, Geology: doi:10.1130/G36377.1; data at: http://www.ncdc.noaa.gov/paleo/study/17635))
    • O2kLR 009.temperature  + (Assemblage not used, chronology is not QC'd)
    • Arc 021.thickness  + (Based on studies of glacier mass balance a …
      Based on studies of glacier mass balance and glaciology in Iceland (e.g. Bjornsson; Flowers), Icelandic glacier fluctuations are dominantly controlled by changes in melt season temperature. Glacier fluctuations influence the production and transport of eroded material and the eventual deposition of this sediment in a downstream basin (i.e. a proglacial lake). ... On short timescales (seasonal, annual, inter-annual), changes in sediment accumulation can be driven by many factors and we can all agree that identifying individual controls is messy. But on longer timescales (for example, centennial timescales, ... I would argue strongly that changes in sediment accumulation are driven by changes in glacier size. This is laid out in Larsen et al., 2011 QSR. We subsequently expanded on this initial study to: 1) include the whole Holocene (Larsen et al., 2012 QSR attached, which demonstrates a clear "8.2ka-event" signal and subsequent Neoglacial onset), and 2) by measuring varve thickness in multiple cores along a lake transect and tying the core data to seismic stratigraphy (Larsen et al. 2013 EPSL attached). This latter work demonstrates that the trends in sediment accumulation are consistent and observed throughout the lake basin. Given the available data, I feel comfortable summarizing as follows: Icelandic glacier fluctuations are dominantly controlled by summer temperature. On longer timescales, fluctuations of the Langjokull ice cap can be reconstructed from changes in mean varve thickness at glacial lake Hvitarvatn. Previous comment: QC failed: article states "sediment flux to Hvítárvatn is dominantly controlled by the integrated rate of sediment production by erosion beneath Langjökull, modulated on annual to decadal timescales by the efficiency of the subglacial fluvial sediment delivery system.", variability function of proximity, absolute values function of sediment availability. This is _not_ temperature!; QQ by PF not passed
      is _not_ temperature!; QQ by PF not passed)
    • Eur 006.temperature  + (By refining dendroclimatological methods the time-series were composited to a mean series and calibrated (1756_1841; r2 = 66%) against Stockholm January_April temperatures.)
    • Aus 041.temperature  + (Calibrated temperature reconstruction from 2006 JQS paper. Elevation estimated from GoogleEarth; rounded to 100 m)
    • Aus 057.temperature  + (Calibrated temperature reconstruction from 2006 JQS paper. Elevation estimated from GoogleEarth; rounded to 100 m)
    • Eur 005.temperature  + (Calibrating and verifying the MXD chronologies against the instrumental temperature data showed a promising opportunity to reconstruct warm-season (May through September) temperature variability)
    • Aus 020.trsgi  + (Composite series, primarily winter T signal. Elevation estimated from GoogleEarth; rounded to 100 m)
    • Aus 015.trsgi  + (Composite series, spring T signal. Elevation estimated from GoogleEarth; rounded to 100 m)
    • LPDbff7f105.R650 700  + (Correlation with temperature is negative, not positive as reported in the publication. An erratum is in press.)
    • Can1101.trsgi  + (Data directly taken from 2013 NatGeo paper, already shifted by 1 year to match seasonality, RCS detrending)
    • Ant 022.dD  + (Data for past 1000 years from https://www. …
      Data for past 1000 years from https://www.ncdc.noaa.gov/paleo/study/14201; data for first millennium CE from https://www.ncdc.noaa.gov/paleo/study/13954 (centennial resolution) plus this study (annual resolution). JRI ice core also has a melt-layer record covering 1000 - 2007 CE http://www.ncdc.noaa.gov/paleo/study/14201
      http://www.ncdc.noaa.gov/paleo/study/14201)
    • Asia 317.temperature  + (Decadal resolution. Elevation estimated from GoogleEarth; rounded to 100 m)
    • Asia 319.temperature  + (Decadal resolution. Elevation estimated from GoogleEarth; rounded to 100 m)
    • Asia 320.temperature  + (Decadal resolution. Elevation estimated from GoogleEarth; rounded to 100 m)
    • Asia 324.temperature  + (Decadal resolution. Elevation estimated from GoogleEarth; rounded to 100 m)
    • Asia 325.temperature  + (Decadal resolution. Elevation estimated from GoogleEarth; rounded to 100 m)
    • Asia 327.temperature  + (Decadal resolution. Elevation estimated from GoogleEarth; rounded to 100 m)
    • Asia 328.temperature  + (Decadal resolution. Elevation estimated from GoogleEarth; rounded to 100 m)
    • NAm 1384.trsgi  + (Decent correlation, but EPS drops below 0.85 near present)
    • Ocean2kHR 160.d18O  + (Duplicate of modern d18O record presented in Cobb et al 2001, 2003 (Ocean2kHR_139))
    • NAm 1924.trsgi  + (EPS drops below arbitrary 0.85 level in early 1700s, but otherwise looks good…)
    • NAm 1468.MXD  + (EPS is variable, but this is a long record with a good climate signal)
    • NAm 2596.trsgi  + (Early series distortion due to low sample number)
    • NAm 364.trsgi  + (Early series problems)
    • NAm 064.trsgi  + (Early series sample depth problems)
    • Arc 008.trsgi  + (Elevation estimated from GoogleEarth; rounded to 100 m)
    • Asia 049.trsgi  + (Elevation estimated from GoogleEarth; rounded to 100 m)
    • Asia 050.trsgi  + (Elevation estimated from GoogleEarth; rounded to 100 m)
    • Asia 051.trsgi  + (Elevation estimated from GoogleEarth; rounded to 100 m)
    • Asia 052.trsgi  + (Elevation estimated from GoogleEarth; rounded to 100 m)
    • Asia 053.trsgi  + (Elevation estimated from GoogleEarth; rounded to 100 m)
    • Asia 054.trsgi  + (Elevation estimated from GoogleEarth; rounded to 100 m)
    • Asia 055.trsgi  + (Elevation estimated from GoogleEarth; rounded to 100 m)
    • Asia 056.trsgi  + (Elevation estimated from GoogleEarth; rounded to 100 m)
    • Asia 057.trsgi  + (Elevation estimated from GoogleEarth; rounded to 100 m)
    • Asia 058.trsgi  + (Elevation estimated from GoogleEarth; rounded to 100 m)
    • Asia 059.trsgi  + (Elevation estimated from GoogleEarth; rounded to 100 m)
    • Asia 060.trsgi  + (Elevation estimated from GoogleEarth; rounded to 100 m)
    • Asia 061.trsgi  + (Elevation estimated from GoogleEarth; rounded to 100 m)
    • Asia 067.trsgi  + (Elevation estimated from GoogleEarth; rounded to 100 m)
    • Asia 068.trsgi  + (Elevation estimated from GoogleEarth; rounded to 100 m)
    • Asia 069.trsgi  + (Elevation estimated from GoogleEarth; rounded to 100 m)
    • Asia 070.trsgi  + (Elevation estimated from GoogleEarth; rounded to 100 m)
    • Asia 071.trsgi  + (Elevation estimated from GoogleEarth; rounded to 100 m)
    • Asia 074.trsgi  + (Elevation estimated from GoogleEarth; rounded to 100 m)
    • Asia 075.trsgi  + (Elevation estimated from GoogleEarth; rounded to 100 m)
    Retrieved from "https://wiki.linked.earth/Special:SearchByProperty/:QCnotes/3-2Dyear-20smoothed"