Rock-N: a potential feedback to the Earth System · Rock-N weathering - determined by denudation...
Transcript of Rock-N: a potential feedback to the Earth System · Rock-N weathering - determined by denudation...
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Rock-N: a potential feedback to the Earth System
Pawlok Dass, Benjamin Z. Houlton, Scott MorfordHoulton Lab, UC Davis
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Nitrogen from rock weathering (Rock-N) (weathering model)
Terrestrial Productivity (GPP)
?
(LPJ-GUESS)
Climate
Hypothesis
Feedback considered in this study
Feedback not considered in this study
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Rock-N weathering - determined by denudationWhich is a function of (see Houlton et al., in review, Science):
● Geochemistry - lithological map
● Relief - digital elevation map
● Tectonic uplift - 10Be (cosmogenic radiation)
● Climate - Excess water and Evapotranspiration maps
● Biology - not implemented yet
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Rock-N & NDEP (atmos. N deposition) global totals
NDEP Rock-N
Whole world
67.9 TgN 16.2 TgN
Natural veg (2009)
45.3 TgN 12.2 TgN
For Natural vegetation only, classes masked out: Water, Permanent wetlands, Croplands, Urban and built up, Cropland and natural vegetation mosaic
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NDEP & Rock-N distribution (current values)
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Climate change
RCP 8.5 → 8.5 W/m2 (by 2100) → 3.7 °C warming (2100) → business as usual
RCP 2.6 → 2.6 W/m2 (by 2100) → 1.0 °C warming (2100) → aggressive mitigation
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Rock-N & NDEP - changes with climate
Fig: Atmospheric N deposition with climate Fig: Atmospheric N deposition with climate
Previously accounted for
Previously unaccounted for
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Climate change and Rock-N (spatial change)
Rock-N change: RCP 8.5 Rock-N change: RCP 2.6
Figs: Change of Rock-N from 1901 to 2101 demonstrated by trend values (in kgN/m2/yr). BLUE: increase in Rock-N; RED: decrease in Rock-N
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Gross Primary Productivity(GPP)
- using LPJ-GUESS
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GPP - changes with climate
2.45 PgC
2.20 PgC
3.13 PgC
Fig: GPP (global total) changes with climate Fig: Δ GPP (global total) only due to Rock-N
Business as usual
High mitigation
Business as usual
High mitigation
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GPP gains only due to Rock-N (ΔGPP)
ΔGPP: RCP 8.5ΔGPP: RCP 2.6
Figs: Trend 1901-2101 (gC/m2/yr)
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GPP: difference with observation“All models are wrong” - George Box
RED: Pixels (areas) where LPJ-GUESS is underperforming with respect to observation
HYPOTHESIS: On addition of Rock-N total RED area (model underperformance) will reduce.
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GPP: Rock-N decreasing model-observation disagreement
Simulations FLUXNET MODIS
LPJ [NDEP + Nfix] 35.15 30.27
LPJ [RockN + NDEP + Nfix] 33.47 28.78
Decrease 1.68 1.49
Table: % of area (vegetated ice free land) where simulated GPP is less than observed GPP
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Scope for improvement
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1. Compute an upper bound for ΔGPP
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2. Permafrost: freeze-thaw weathering
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2. Permafrost: freeze-thaw weathering
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3. Mycorrhizae: active Rock-N uptake
Thin-section micrograph of feldspar grain
Landwert et al., 2001Thin-section micrograph
of feldspar grain Sholl et al., 2008
Scanning electron micrograph
Sholl et al., 2008
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Summary● Nitrogen from rock weathering (Rock-N) accounts for a significant increase in
terrestrial productivity.
● The increase in productivity shown here is probably a conservative estimate.
● The high latitudes are probably not as Nitrogen limited as previously thought.
● Increase in productivity due to Rock-N has the potential to act as a negative
feedback.
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Other Carbon cycle values
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Impact of Rock-N: other C-cycle valuesNPP
0.92 PgC
0.95 PgC
0.78 PgC
Rh
0.67 PgC
0.56 PgC
0.61 PgC
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Impact of Rock-N: other C-cycle valuesNEE
0.26 PgC
0.34 PgC
0.22 PgC
Fire emissions
0.21 PgC
0.21 PgC
0.33 PgC
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Impact of Rock-N: other C-cycle valuesNBP
0.05 PgC
0.01 PgC
0.01 PgC
Total C-pool
54.26 PgC
58.78 PgC
59.32 PgC