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Hourly and daily rainfall intensification causes opposing effects on C and N emissions, storage, and leaching in dry and wet grasslands

TLDR
In this paper, the authors investigate the effects of expected twenty-first century changes in hourly and daily rainfall on soil carbon and nitrogen emissions, soil organic matter (SOM) stocks, and leaching using a coupled mechanistic soil biogeochemical model (BAMS2).
Abstract
Climate change is expected to alter hourly and daily rainfall regimes and, in turn, the dynamics of ecosystem processes controlling greenhouse gas emissions that affect climate. Here, we investigate the effects of expected twenty-first century changes in hourly and daily rainfall on soil carbon and nitrogen emissions, soil organic matter (SOM) stocks, and leaching using a coupled mechanistic carbon and nitrogen soil biogeochemical model (BAMS2). The model represents various abiotic and biotic processes involving 11 SOM pools. These processes include fungal depolymerization, heterotrophic bacterial mineralization, nitrification, denitrification, microbial mortality, necromass decomposition, microbial response to water stress, protection, aqueous advection and diffusion, aqueous complexation, and gaseous dissolution. Multi-decadal modeling with varying rainfall patterns was conducted on nine Australian grasslands in tropical, temperate, and semi-arid regions. Our results show that annual $${\text{CO}}_2$$ emissions in the semi-arid grasslands increase by more than 20% with a 20% increase in annual rainfall (with no changes in the rainfall timing), but the tropical grasslands have opposite trends. A 20% increase in annual rainfall also increases annual $${\text{N}}_2{\text{O}}$$ and NO emissions in the semi-arid grasslands by more than 10% but decreases emissions by at least 25% in the temperate grasslands. When subjected to low frequency and high magnitude daily rainfall events with unchanged annual totals, the semi-arid grasslands are the most sensitive, but changes in annual $${\text{CO}}_2$$ emissions and SOM stocks are less than $$5\%$$ . Intensification of hourly rainfall did not significantly alter $${\text{CO}}_2$$ emissions and SOM stocks but changed annual $${\text{NH}}_3$$ emissions in the tropical grasslands by more than 300%.

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Lawrence Berkeley National Laboratory
Recent Work
Title
Hourly and daily rainfall intensification causes opposing effects on C and N emissions,
storage, and leaching in dry and wet grasslands
Permalink
https://escholarship.org/uc/item/0zs3r5jb
Journal
Biogeochemistry, 144(2)
ISSN
0168-2563
Authors
Tang, FHM
Riley, WJ
Maggi, F
Publication Date
2019-07-30
DOI
10.1007/s10533-019-00580-7
Peer reviewed
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University of California

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&8'-+++1D-+;A:%

8%-+;-:/
$$&
82-+;A1B-+;5:
8E-+;F:7
&3&
&8C-++A1G
-+;61?-+;6:8G-++61(
-+;F:$82/*=<-+;A1
*-+;,:89
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5
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1
-++,1B-+;-:<7
&$$
C8(9:
7$
9(9
<<$
8(-++6:$8<-+;-:
9
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97
=/9
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$383
HBirch eectI*;4,F1#-+;+1J-+;+:(
$/7&
&&$
$$&9
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8(-+;F:
$$$
8B;4F6:$<$$8&/EK-+;-:
$8-+;5:$
8C-+;-:7&
/L7
$&//$
@$&
(9&
829:$82@:8#-+;F:9
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M7$
$$8**-+++:1
=2@
<$7
3&$
8*-+;-13*;4441

<C-++4:J
$&&
$$8E!-+;+1(
-+;F:&$$(9
<$$<$
$82?3-+;-:3$8##N-+;5:
8-+;6:8**-++,1(3
;44,:8#;44-1
(7;4F,1!-+++:$&
3&/
8-++F1((-++5:<
82?3-+;-:@L
$
$3$$&
97$
8#=;4441#-++5:$
$&&8C
-+;-1*-+;,:=
7&(9
&=/
&$

*%(;&!
8-+;5:&8-++F:$
&(9
O8*%(-1*%$(9
&-:;;(98&
:&$8$
77:3
$=
&=7
*%(-$3/$&
1
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991$1
3
7
&%
/

*%(-3

&$(9
*%(;$$!8-+;5:
&8-++F:O
38*%(-;:(98
:1&(9
8
:1&8
A
 
9
-
9
-
:1&$
8F
DEP
:$8B
HET
:/7<
$8B
AOB
:/7<$8B
NOB
:$
8B
DEN
:
@*%(- $(98!;O!F
;:%$$$
$&"F,&
8-+;5:@</8!4O
!;;:<$$
& 
$$F
DEP
B
HET
(97<$B
AOB
 
3$(9
*%(;8!-+;5:
$<$$
8(@$(;:
(8!;-O!;A:
8!;5O!;6:8-++F:
$$
$$8($(;:@
*%(-
-
7 8!;4:%!;4
$7
-
7$
7$
-
7$&
$=17$$
$$
8!-+;;:
C3$  8!-+O!-;:$&
8!-FO!-4"A,-++;1
%3;44A:$8!-67"

Citations
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Soil Organic Matter Research and Climate Change: Merely Re-storing Carbon Versus Restoring Soil Functions

TL;DR: In this paper, the authors argue that a far better strategy revolves around the effect of climate change on functions/services that soils render, since climatologists forecast less frequent but more intense rainfall events in the future, which may lead to food shortages, catastrophic flooding and soil erosion if soils are not able to cope.

Detection of spatially aggregated changes in temperature and precipitation extremes

TL;DR: In this article, the authors used a spatially aggregated perspective to detect a distinct intensification of heavy precipitation events and hot extremes and showed that much of the local to regional differences in trends of extremes can be explained by internal variability, which can regionally mask or amplify the forced long-term trends.
Journal ArticleDOI

Abiotic and Biotic Controls on Soil Organo–Mineral Interactions: Developing Model Structures to Analyze Why Soil Organic Matter Persists

TL;DR: In this article, the conundrum as to why some SOM decomposes rapidly, while other thermodynamically unstable SOM can persist on centennial time scales leads to substantial uncertainty in model structures, as well as uncertainty in the predictability of the land carbon sink trajectory.

Microbial Soil Respiration and its dependency on Carbon Inputs, Soil Temperature and Moisture in two contrasting ecosystems

TL;DR: In this article, three determinant factors in decomposition patterns of soil organic matter (SOM): temperature, water and carbon (C) inputs were studied. But the authors focused on the role of the above-defined environmental factors on the variability of soil C dynamics.
Journal ArticleDOI

Rainfall intensification increases the contribution of rewetting pulses to soil heterotrophic respiration

TL;DR: In this article, a stochastic model for soil heterotrophic respiration rates was developed, which analytically links the statistical properties of respiration to those of precipitation, and showed that both the mean rewetting pulse respiration and the mean respiration during drying increase with increasing mean precipitation.
References
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Anaerobic ammonium oxidation discovered in a denitrifying fluidized bed reactor

TL;DR: Anaerobic ammonium oxidation is a new process in which ammonium is oxidized with nitrate serving as the electron acceptor under anaerobic conditions, producing dinitrogen gas, and has been given the name ‘Anammox’ (anaerobic ammonia oxidation), and has be patented.
Journal ArticleDOI

An Overview of the Global Historical Climatology Network-Daily Database

Abstract: A database is described that has been designed to fulfill the need for daily climate data over global land areas. The dataset, known as Global Historical Climatology Network (GHCN)-Daily, was developed for a wide variety of potential applications, including climate analysis and monitoring studies that require data at a daily time resolution (e.g., assessments of the frequency of heavy rainfall, heat wave duration, etc.). The dataset contains records from over 80 000 stations in 180 countries and territories, and its processing system produces the official archive for U.S. daily data. Variables commonly include maximum and minimum temperature, total daily precipitation, snowfall, and snow depth; however, about two-thirds of the stations report precipitation only. Quality assurance checks are routinely applied to the full dataset, but the data are not homogenized to account for artifacts associated with the various eras in reporting practice at any particular station (i.e., for changes in systematic...
Journal ArticleDOI

A model of nitrous oxide evolution from soil driven by rainfall events: 1. Model structure and sensitivity

TL;DR: In this paper, a rain-event driven, process-oriented model of nitrogen and carbon cycling processes in soils was used to simulate N2O and CO2 emissions from soils.
Journal ArticleDOI

The effect of soil drying on humus decomposition and nitrogen availability

H. F. Birch
- 01 Sep 1958 - 
TL;DR: In this paper, the authors show that when a dry soil is moistened, a characteristic pattern of decomposition occurs in which an initial period of relatively rapid decomposition (Stage 1) falls, during a few days, to a slow steady rate (Stage 2).
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Q1. What are the contributions in "Hourly and daily rainfall intensification causes opposing effects on c and n emissions, storage, and leaching in dry and wet grasslands" ?

Here, the authors investigate the effects of expected twenty-first century changes in hourly and daily rainfall on soil carbon and nitrogen emissions, soil organic matter ( SOM ) stocks, and leaching using a coupled mechanistic carbon and nitrogen soil biogeochemical model ( BAMS2 ).