campbell 2015 lter asm v0.1 quest
TRANSCRIPT
Uncertainty in the net hydrologic flux of calcium in a paired-watershed
harvesting study
LTER ASM Estes Park, COSeptember 2015
John Campbell, Ruth Yanai, Mark Green, Genen Likens, Craig See, Amey Bailey, Don Buso, Daqing Yang
Paired watershed studies
W6W5
• Watersheds are unreplicated
• It’s difficult to find suitable replicate watersheds and expensive
• Uncertainty analysis can be used to report statistical confidence
Ca response to harvesting
HarvestHarvest
Data courtesy G.E. Likens
Sources of uncertaintyPrecipitation • Interpolation model• Collector efficiency• Gaps in volume• Chemical analysis• Unusable chemistry
Stream water• Watershed area• Stage height-discharge• Gaps in discharge• Chemical analysis• Interpolation model
May 1956
Precipitation interpolation method
W1 W2 W3 W4 W5 W6 W7 W8 W9
Ann
ual p
reci
p. (m
m)
1340
1360
1380
1400
1420
1440
1460
1480
1500
1520ThiessenKrigingIDWSplineRegression
Uncertainty = 0.6%
Watershed area
W6
Uncertainty = 2.3%
Streamflow
Monte Carlo approach
Chemical value
Net Hydrologic Flux
Etc.
Calculation
Ca response to harvesting
Contributions to Uncertainty
Chemical analyses
Uncertainty = 1.0%
• Precision describes the variation in replicate analysis of the same sample
• At Hubbard Brook, one sample of every 40 is analyzed four times
Acknowledgments
Calcium data were obtained through funding from the A.W. Mellon Foundation and the NSF, including LTER and LTREB.
Amey BaileyIan HalmNick GrantTammy WoosterBranda Minicucci
Gaps in streamflow
• 7% of streamflow record is gaps• 65% due to the cart recorder (50% clock)
Uncertainty = 7.9%
Easier said than done…
• Difficult to identify sources of uncertainty
• Difficult to quantify sources
• Multiple approaches to uncertainty analysis
• No single answer
Water year (June 1)1960 1970 1980 1990 2000 2010
Net
hyd
rolo
gic
flux
(kg
ha-1
yr-
1)
-24
-21
-18
-15
-12
-9
-6
-3
0
W6 (reference)W5 (harvested)
Source of excess Ca in W5
• Dissolution of calcium oxalate, which is common in plant tissue and is known to accumulate in forest soils (Bailey et al. 2002).
• Dissolution of nonsilicate minerals, such as calcite and apatite, which are more rapidly weathered than silicate minerals (Hamburg et al. 2003).
Source of excess Ca in W5