Uncertainty in Forest Carbon
and Nutrient Budgets
Ruth D. Yanai
State University of New York
College of Environmental Science and Forestry
Syracuse NY 13210, USA
Quantifying uncertainty in ecosystem budgets
Precipitation (evaluating monitoring intensity)
Streamflow (filling gaps with minimal uncertainty)
Forest biomass (identifying the greatest sources of uncertainty)
Soil stores (detectable differences)
QUANTIFYING UNCERTAINTY
IN ECOSYSTEM STUDIES
Bormann et al. (1977) Science
How can we assign confidence in ecosystem
nutrient fluxes?
Bormann et al. (1977) Science
The N budget for Hubbard Brook published
in 1977 was “missing” 14.2 kg/ha/yr
Net N gas exchange = sinks – sources =
- precipitation N input
+ hydrologic export
+ N accretion in living biomass
+ N accretion in the forest floor
± gain or loss in soil N stores
- weathering N input
The N budget for Hubbard Brook published
in 1977 was “missing” 14.2 kg/ha/yr
14.2 ± ?? kg/ha/yr
The N budget for Hubbard Brook published
in 1977 was “missing” 14.2 kg/ha/yr
14.2 ± ?? kg/ha/yr
Measurement Uncertainty Sampling Uncertainty
Spatial and Temporal Variability
Model Uncertainty
Error within models Error between models
Volume = f(elevation, aspect): 3.4 mm
Undercatch: 3.5%
Chemical analysis: 0-3%
Model selection: <1%
Across
catchments:
3%
Across years:
14%
We tested the effect of sampling intensity by sequentially omitting
individual precipitation gauges.
Estimates of annual precipitation volume varied little until five or more
of the eleven precipitation gauges were ignored.
The N budget for Hubbard Brook published
in 1977 was “missing” 14.2 kg/ha/yr
14.2 ± ?? kg/ha/yr
The N budget for Hubbard Brook published
in 1977 was “missing” 14.2 kg/ha/yr
14.2 ± ?? kg/ha/yr
Gaps in the discharge record are filled by
comparison to other streams at the site,
using linear regression.
S5
S12
S16
S17
S20
0
100
200
0 100 200
0
100
200
300
0 100 200 300
0
50
100
150
0 50 100 150
0
50
100
150
0 50 100 150
0
50
100
0 50 100
Cross-validation: Create fake gaps and
compare observed and predicted discharge
Yanai et al. (2014)
Hydrological Processes
Net N gas exchange = sinks – sources =
- precipitation N input (± 1.3)
+ hydrologic export (± 0.5)
+ N accretion in living biomass
+ N accretion in the forest floor
± gain or loss in soil N stores
The N budget for Hubbard Brook published
in 1977 was “missing” 14.2 kg/ha/yr
14.2 ± ?? kg/ha/yr
Net N gas exchange = sinks – sources =
- precipitation N input (± 1.3)
+ hydrologic export (± 0.5)
+ N accretion in living biomass
+ N accretion in the forest floor
± gain or loss in soil N stores
The N budget for Hubbard Brook published
in 1977 was “missing” 14.2 kg/ha/yr
14.2 ± ?? kg/ha/yr
Tree Inventory
log(Height) = a + b*log(Diameter) ± error
log (Mass) = a + b*log(1/2 r2
*Height) ± error
Nutrient content = Mass * (Concentration ± error)
Sum all trees and all tissue types
Allometric Equations
and Nutrient Concentrations
Monte Carlo
Simulation
Yanai, Battles, Richardson, Rastetter,
Wood, and Blodgett (2010) Ecosystems
Monte Carlo simulations use
random sampling of the
distribution of the inputs to a
calculation. After many
iterations, the distribution of the
output is analyzed.
611 ± 54 kg N/ha
Nitrogen Content of Biomass
with Uncertainty
***IMPORTANT***
Random selection of parameter
values applies across all the
trees and all the time periods in
each iteration.
The uncertainty between two
measurements can be less than
in a single measurement!
Net N gas exchange = sinks – sources =
- precipitation N input (± 1.3)
+ hydrologic export (± 0.5)
+ N accretion in living biomass (± 1)
+ N accretion in the forest floor
± gain or loss in soil N stores
The N budget for Hubbard Brook published
in 1977 was “missing” 14.2 kg/ha/yr
14.2 ± ?? kg/ha/yr
Net N gas exchange = sinks – sources =
- precipitation N input (± 1.3)
+ hydrologic export (± 0.5)
+ N accretion in living biomass (± 1)
+ N accretion in the forest floor
± gain or loss in soil N stores
The N budget for Hubbard Brook published
in 1977 was “missing” 14.2 kg/ha/yr
14.2 ± ?? kg/ha/yr
Nitrogen in the Forest Floor
Hubbard Brook Experimental Forest
y = 0 .0 0 0 2 x - 0 . 1 6 1 9
R 2
= 0 . 0 1 0 9
0
0 . 0 5
0 .1
0 . 1 5
0 .2
0 . 2 5
1 9 7 5 1 9 8 0 1 9 8 5 1 9 9 0 1 9 9 5 2 0 0 0 2 0 0 5
ForestFloorN(kg/m2)
The change is insignificant (P = 0.84).
The uncertainty in the slope is ± 22 kg/ha/yr.
Net N gas exchange = sinks – sources =
- precipitation N input (± 1.3)
+ hydrologic export (± 0.5)
+ N accretion in living biomass (± 1)
+ N accretion in the forest floor (± 22)
± gain or loss in soil N stores
The N budget for Hubbard Brook published
in 1977 was “missing” 14.2 kg/ha/yr
14.2 ± ?? kg/ha/yr
Studies of soil change over time often fail to detect a difference.
We should always report how large a difference is detectable.
Yanai et al. (2003) SSSAJ
Power analysis can be used to determine the
difference detectable with known confidence
Yanai et al. (2003) SSSAJ
Sampling the same experimental units over time
permits detection of smaller changes
Yanai et al. (2003) SSSAJ
In this analysis of forest floor studies,
few could detect small changes
Yanai et al. (2003) SSSAJ
Net N gas exchange = sinks – sources =
- precipitation N input (± 1.3)
+ hydrologic export (± 0.5)
+ N accretion in living biomass (± 1)
+ N accretion in the forest floor (± 22)
± gain or loss in soil N stores
The N budget for Hubbard Brook published
in 1977 was “missing” 14.2 kg/ha/yr
14.2 ± ?? kg/ha/yr
Nitrogen Pools (kg/ha)
Hubbard Brook Experimental Forest
1796
29
10
1260
750
3080
Forest Floor
Live Vegetation
Coarse Woody Debris
Mineral Soil
10 cm-C
Dead Vegetation
Mineral Soil
0-10 cm
Yanai et al. (2013) ES&T
We can’t detect a difference of 730 kg N/ha in the mineral soil.
From 1983 to 1998, 15 years post-harvest, there was an
insignificant decline of 54 ± 53 kg N ha-1
y-1
Huntington et al. (1988)
Yanai et al. (2013) ES&T
Net N gas exchange = sinks – sources =
- precipitation N input (± 1.3)
+ hydrologic export (± 0.5)
+ N accretion in living biomass (± 1)
+ N accretion in the forest floor (± 22)
± gain or loss in soil N stores (± 53)
The N budget for Hubbard Brook published
in 1977 was “missing” 14.2 kg/ha/yr
14.2 ± ?? kg/ha/yr
Net N gas exchange = sinks – sources =
- precipitation N input (± 1.3)
+ hydrologic export (± 0.5)
+ N accretion in living biomass (± 1)
+ N accretion in the forest floor (± 22)
± gain or loss in soil N stores (± 53)
The N budget for Hubbard Brook published
in 1977 was “missing” 14.2 kg/ha/yr
14.2 ± 57 kg/ha/yr
Net N gas exchange = sinks – sources =
- precipitation N input (± 1.3)
+ hydrologic export (± 0.5)
+ N accretion in living biomass (± 1)
The N budget for Hubbard Brook published
in 1977 was “missing” 14.2 kg/ha/yr
14.2 ± 2.6 kg/ha/yr
Draw your budget boundaries to ask questions
that can be answered with confidence!
The Value of Uncertainty Analysis
Quantify uncertainty in our results
Uncertainty in regression
Monte Carlo sampling
Detectable differences
Identify ways to reduce uncertainty
Devote effort to the greatest unknowns
Improve efficiency of monitoring efforts
Be a part of QUEST!
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QUANTIFYING UNCERTAINTY
IN ECOSYSTEM STUDIES
References
Yanai, R.D., N. Tokuchi, J.L. Campbell, M.B. Green, E. Matsuzaki, S.N. Laseter, C.L.
Brown, A.S. Bailey, P. Lyons, C.R. Levine, D.C. Buso, G.E. Likens, J. Knoepp, K.
Fukushima. 2014. Sources of uncertainty in estimating stream solute export from
headwater catchments at three sites. Hydrological Processes. DOI: 10.1002/hyp.10265
Yanai, R.D., M.A. Vadeboncoeur, S.P. Hamburg, M.A. Arthur, M.A. Fuss, P.M.Groffman,
T.G. Siccama, and C.T. Driscoll. 2013. From Missing Source to Missing Sink: Long-
Term Changes in a Forest Nitrogen Budget. Environmental Science & Technology.
47(20):11440-11448.
Yanai, R.D., C.R. Levine, M.B. Green, and J.L. Campbell. 2012. Quantifying uncertainty
in forest nutrient budgets, J. For. 110: 448-456
Yanai, R.D., J.J. Battles, A.D. Richardson, E.B. Rastetter, D.M. Wood, and C. Blodgett.
2010. Estimating uncertainty in ecosystem budget calculations. Ecosystems 13: 239-248
Wielopolski, L, R.D. Yanai, C.R. Levine, S. Mitra, and M.A Vadeboncoeur. 2010.
Rapid, non-destructive carbon analysis of forest soils using neutron-induced gamma-ray
spectroscopy. For. Ecol. Manag. 260: 1132-1137
Yanai, R.D., S.V. Stehman, M.A. Arthur, C.E. Prescott, A.J. Friedland, T.G. Siccama, and
D. Binkley. 2003. Detecting change in forest floor carbon. Soil Sci. Soc. Am. J. 67:1583-
1593
My web site: www.esf.edu/faculty/yanai (Download any papers)
QUEST, NSF RCN. Outline of the talk: Parts of the ecosystem budget, each illustrating an application of uncertainty analysis. These applications are relevant to all of us involved in forest measurements and management, even if you’re not interested in nutrient budgets per se.
The same principles apply to C budgets
This was the first N budget for HB, published in 1977. Say that it’s an impressive achievement. Quantifying all the pools, and all the sources and sinks. They didn’t add up, there was an imbalance between the sources and sinks…
There was 14.2 kg/ha/yr missing. 14 point two? Plus or minus what?
I started my dissertation at Hubbard Brook in 1983, working on the P budget, and for 25 years it troubled me that we couldn’t assign uncertainty in forest ecosystem budgets.
Put back the animated version
For each of these sources or sinks, I have a diagram illustrating the sources of uncertainty. (Make sure this connects to the estimate in the budget mass balance.)
Figure 7. Sources of uncertainty in stream export of nutrients, illustrated with values for streams at the Hubbard Brook Experimental Forest, except for uncertainty due to gaps of 1-2 weeks in stream discharge at Wakayama, Japan (Tokuchi, Fukushima, and Matsuzaki, personal communication). Uncertainty in stage height is the effect on annual flux of the uncertainty in weekly readings. Sampling uncertainty describes the range in runoff variability for 2000-2009. The height-discharge relationship is calibrated only at low flow; uncertainty at high flows may be very large. Model selection error is for the long-term average export of calcium and nitrate.
The weir cover that protects the basin heater was demolished by an ice-flow that bulldozed virtually the entire stream channel above the gauging station basin on 6 March 2011. The ice flow was produced by a rain-on-snow event and the presence of a thick ice layer on the stream, which allowed the frozen slurry to run down the hillslope un-checked, scouring the channel on the way to the weir. There is a boulder the size of table in the basin. The weir data were missing for about 3 weeks, until the ice could be removed from the V-notch and the floats re-calibrated to the notch height. During that period data from nearby W8 and W7 were used to model the flows in W9. The regression model is based on 15 years of continuous, parallel discharge measurements. Severe incidents of this sort are rare: this is the second time I have seen this in 37 years.
Replace this with gaps at Hubbard Brook
At Wakayama, Japan, gaps of Gaps of 1-3 days resulted in less than 0.5% error in the annual estimate of flow (Figure 6). Gaps of 1-2 weeks gave an average error of 1% of annual flow. Longer gaps still resulted in &lt;2% error, except for two long gaps of 2 or 3 months that gave errors of 7-8% (Figure 6).
I put in 0.5, based on the current low values of N export (0.8 kg/ha/yr) and the variation across replicate streams.
This is not a very certain number, stay tuned
I put in 0.5, based on the current low values of N export (0.8 kg/ha/yr) and the variation across replicate streams.
This is not a very certain number, stay tuned
The biomass calculation is really complicated. We have a complete inventory of every tree on the watershed (actually, this simplifies things; we have no sampling error). We have allometric equations relating tree height to tree diameter, by species and biomass of tissues (bark, branches, leaves, wood, roots) to the parabolic volume of the tree, which we get from the height and diameter. Then we have tissue concentrations for each species and tissue type. So we propagate the uncertainty in measurement error, regression, and concentration using a Monte Carlo approach.
Rather than do anything analytical (like a Gaussian approach)
Here are 100 values, you can see the variation
Graph the variation. But this is not what we want, we want change over time.
Uncertainty at one point in time was 54. Paired, 5
Uncertainty at one point in time was 54
At Hubbard Brook, Whittaker’s equations have very small errors. Will Oswaldo talk about equations in Mexico?
Emphasize model selection error
Divide by 5 years, we get plus or minus 1. This value I’m very confident of. It ranges from .5 to .9, depending on the period
Divide by 5 years, we get plus or minus 1. This value I’m very confident of. It ranges from .5 to .9, depending on the period
Divide by 5 years, we get plus or minus 1. This value I’m very confident of. It ranges from .5 to .9, depending on the period
Power to detect different magnitudes of change in forest floor organic mass for various sample sizes, using the variance of paired differences measured in a regional study of 30 stands (Friedland et al., 1992)
The sample size required to detect a given % change with power = 0.75. The three curves represent different levels of variability derived from Friendland et al. (1992), w upper and lower bounds of the 95% CI for the SD of the differences.
Frequency distribution of detectable change in 21 studies (some are represented more than once, paired an independent or plots vs. stands)
Divide by 5 years, we get plus or minus 1. This value I’m very confident of. It ranges from .5 to .9, depending on the period
The summary;
The depth distribution of fine root biomass depends on root diameter and forest type as a Ca gradient.
The finer roots are more concentrated at the shallow depth in the high Ca availability.
Roots larger than 0.5 mm in hardwoods don’t depend on soil depth and Ca availability, but those of softwoods decrease as soil depth and Ca availability.
Dead roots are more in softwoods than hardwoods, especially the most at low Ca available site.
There are no difference in live and dead root biomass among sites in hardwoods, but highest in Cone Pone in softwoods.
Divide by 5 years, we get plus or minus 1. This value I’m very confident of. It ranges from .5 to .9, depending on the period
Don’t despair. Without the soil, the uncertainty is 2.6. We can say with great confidence that there was a missing source in the N budget (now, instead, we have a missing sink).
Add a conclusion slide: draw your budget boundaries carefully to ask questions that can be answered with confidence.
Don’t despair. Without the soil, the uncertainty is 2.6. We can say with great confidence that there was a missing source in the N budget (now, instead, we have a missing sink).
Add a conclusion slide: draw your budget boundaries carefully to ask questions that can be answered with confidence.
Put in a plug for our as-yet unfunded RCN. We already have a web site, mailing list of 177. Statistical Advice Bureau of 12 experts willing to collaborate with us.
These are 5 models of precipitation in the HB valley, using built-in models in ARC GIS. We can see that each is interpolating between the rain gauges differently.
When we compare the estimates of the different models for the whole valley, we see that there is low variation between the models. Next, we will be working on how to estimate the uncertainty not just between the models, but also within each model.