Assessment of terrestrial vegetation dynamics from MODIS fAPARchl product and land surface model

2016 ◽  
Author(s):  
Tian Yao ◽  
Qingyuan Zhang
Keyword(s):  
Land Surface ◽  
Vegetation Dynamics ◽  
Land Surface Model ◽  
Surface Model ◽  
Terrestrial Vegetation

scholarly journals Implementation of a Marauding Insect Module (MIM, version 1.0) in the Integrated BIosphere Simulator (IBIS, version 2.6b4) dynamic vegetation–land surface model

2016 ◽  
Vol 9 (3) ◽  
pp. 1243-1261 ◽  
Author(s):  
Jean-Sébastien Landry ◽  
David T. Price ◽  
Navin Ramankutty ◽  
Lael Parrott ◽  
H. Damon Matthews
Keyword(s):  
Land Surface ◽  
Vegetation Dynamics ◽  
Bark Beetles ◽  
Mountain Pine Beetle ◽  
Land Surface Model ◽  
Field Measurements ◽  
Surface Model ◽  
Climatic Effects ◽  
Standing Trees ◽  
Integrated Biosphere Simulator

Abstract. Insects defoliate and kill plants in many ecosystems worldwide. The consequences of these natural processes on terrestrial ecology and nutrient cycling are well established, and their potential climatic effects resulting from modified land–atmosphere exchanges of carbon, energy, and water are increasingly being recognized. We developed a Marauding Insect Module (MIM) to quantify, in the Integrated BIosphere Simulator (IBIS), the consequences of insect activity on biogeochemical and biogeophysical fluxes, also accounting for the effects of altered vegetation dynamics. MIM can simulate damage from three different insect functional types: (1) defoliators on broadleaf deciduous trees, (2) defoliators on needleleaf evergreen trees, and (3) bark beetles on needleleaf evergreen trees, with the resulting impacts being estimated by IBIS based on the new, insect-modified state of the vegetation. MIM further accounts for the physical presence and gradual fall of insect-killed dead standing trees. The design of MIM should facilitate the addition of other insect types besides the ones already included and could guide the development of similar modules for other process-based vegetation models. After describing IBIS–MIM, we illustrate the usefulness of the model by presenting results spanning daily to centennial timescales for vegetation dynamics and cycling of carbon, energy, and water in a simplified setting and for bark beetles only. More precisely, we simulated 100 % mortality events from the mountain pine beetle for three locations in western Canada. We then show that these simulated impacts agree with many previous studies based on field measurements, satellite data, or modelling. MIM and similar tools should therefore be of great value in assessing the wide array of impacts resulting from insect-induced plant damage in the Earth system.

Disentangling the long-term foliar 15N signal using a land surface model

2020 ◽  
Author(s):  
Silvia Caldararu ◽  
Tea Thum ◽  
Richard Nair ◽  
Sönke Zaehle
Keyword(s):  
Nutrient Limitation ◽  
Land Surface ◽  
Nitrogen Availability ◽  
Land Surface Model ◽  
Ecosystem Dynamics ◽  
Surface Model ◽  
Terrestrial Vegetation ◽  
Climate System Model ◽  
Foliar N

<p>Terrestrial vegetation growth is hypothesised to increase under elevated atmospheric CO<sub>2</sub>, a process known as the CO<sub>2</sub> fertilisation effect. However, the magnitude of this effect and its long-term sustainability remains uncertain. One of the main limitations to the CO2  fertilisation effect is nutrient limitation to plant growth, in particular nitrogen (N) in temperate and boreal ecosystems. Recent studies have suggested that decreases in observed foliar N content (N%) and δ<sup>15</sup>N indicate widespread nitrogen limitation with increasing CO<sub>2</sub>  concentrations. However, the factors driving these two variables, and especially the foliar δ<sup>15</sup>N values, are complex and can be caused by a number of processes. On one hand, if the observed trends reflect nutrient limitation, this limitation can be caused by either CO<sub>2</sub> or warming driven growth. On the other hand, it is possible that nutrient limitation does not occur to its full extent due to plant plastic responses to alleviate nutrient limitation, causing a decrease in N%, but changes in the anthropogenic N deposition 15N signal cause the observed δ<sup>15</sup>N trend. In reality, it is likely that all these factors contribute to the observed trends. To understand ecosystem dynamics it is important to disentangle the processes behind these signals which is very difficult based on observational datasets only.</p><p>We use a novel land surface model to explore the causes behind the observed trends in foliar N% and δ<sup>15</sup>N. The QUINCY (QUantifying Interactions between terrestrial Nutrient CYcles and the climate system) model  has the unique capacity to track ecologically relevant isotopic composition, including <sup>15</sup>N in plant and soil pools. The model also includes a realistic representation of plant plastic acclimation processes, specifically a representation of nitrogen allocation to and inside the canopy in response to nitrogen availability, so implicitly to changes in CO<sub>2 </sub> concentrations. We test the different hypotheses above behind the observed changes in N% and δ<sup>15</sup>N separately and quantify the contribution of each of the factors towards the observed trend. We then test the different hypotheses against existing observations of N% and δ<sup>15</sup>N from the ICP Forests database and other published datasets such as the global dataset of Craine et al. 2018.</p><p>Our study showcases the use of an isotope-enabled land surface model in conjunction with long-term observations to strengthen our understanding of the ecosystem processes behind the observed trends.</p>

scholarly journals Modeling the Vegetation Dynamics of Northern Shrubs and Mosses in the ORCHIDEE Land Surface Model

2019 ◽  
Vol 11 (7) ◽  
pp. 2020-2035 ◽  
Author(s):  
Arsène Druel ◽  
Philippe Ciais ◽  
Gerhard Krinner ◽  
Philippe Peylin
Keyword(s):  
Land Surface ◽  
Vegetation Dynamics ◽  
Land Surface Model ◽  
Surface Model

A description of the COS budget inferred by inverse modelling

2021 ◽  
Author(s):  
Marine Remaud ◽  
Camille Abadie ◽  
Sauveur Belviso ◽  
Antoine Berchet ◽  
Frédéric Chevallier ◽  
...  
Keyword(s):  
Land Surface ◽  
Transport Model ◽  
Atmospheric Transport ◽  
Land Surface Model ◽  
Diffusion Path ◽  
Global Scale ◽  
Striking Similarity ◽  
Surface Model ◽  
Terrestrial Vegetation ◽  
The Tropics

<p>Carbonyle Sulphide, a trace gas exhibiting a striking similarity with CO2 in the biochemical diffusion path of leaves, has been recognized to be a promising surrogate of CO2 for estimating carbon storage in the terrestrial vegetation. Based on the similarity between COS and CO2, an empirical linear model relating both gas concentrations provides constraints on the estimation of the Gross Primary Productivity (GPP), the amount of carbon dioxide that is absorbed by ecosystems. However, large uncertainties on the other components of its atmospheric budget prevent us from directly relating the atmospheric COS measurements to the the GPP at global scale. The largest uncertainty arises from the closure of its atmospheric budget, with a source component missing. We explore here the benefit of assimilating both COS and CO2 measurements into the LMDz atmospheric transport model to gain insight on the COS budget. We develop an analytic inverse system which optimized the biospheric fluxes within the 14 Plant functional Type (PFTs) as defined in the ORCHIDEE land surface model. The vegetation uptake of COS is parameterized as a linear function of GPP and of the leaf relative uptake (LRU), which is the ratio of COS to CO2 deposition velocities in plants. A possible scenario leads to a global biospheric sink between 800-900 GgS/y, with a higher GPP in the high latitudes and higher total oceanic emissions between 400 and 600 GgS/y over the tropics. The COS inter-hemispheric gradient is in better agreement with HIPPO independent aircraft measurements. The comparison against NOAA COS airborne profiles and Solar Induced Fluorescence shed light on a too strong GPP in spring in ORCHIDEE in northern America,  leaving room for improvements. <span>We also show that uncertainty in the location of hot spots in the prior anthropogenic inventory limits the use of atmospheric COS measurements in inverse modeling.</span></p>

scholarly journals Exposures to temperature beyond threshold disproportionately reduce vegetation growth in the northern hemisphere

2018 ◽  
Vol 6 (4) ◽  
pp. 786-795 ◽  
Author(s):  
Xiuchen Wu ◽  
Weichao Guo ◽  
Hongyan Liu ◽  
Xiaoyan Li ◽  
Changhui Peng ◽  
...  
Keyword(s):  
Northern Hemisphere ◽  
Land Surface ◽  
Vegetation Index ◽  
Vegetation Type ◽  
Land Surface Model ◽  
Terrestrial Ecosystems ◽  
Surface Model ◽  
Terrestrial Vegetation ◽  
Vegetation Growth ◽  
Temperature Thresholds

Abstract In recent decades, terrestrial vegetation in the northern hemisphere (NH) has been exposed to warming and more extremely high temperatures. However, the consequences of these changes for terrestrial vegetation growth remain poorly quantified and understood. By examining a satellite-based vegetation index, tree-ring measurements and land-surface model simulations, we discovered a consistent convex pattern in the responses of vegetation growth to temperature exposure (TE) for forest, shrub and grass in both the temperate (30°−50° N) and boreal (50°−70° N) NH during the period of 1982−2012. The response of vegetation growth to TE for the three vegetation types in both the temperate and boreal NH increased convergently with increasing temperature, until vegetation type-dependent temperature thresholds were reached. A TE beyond these temperature thresholds resulted in disproportionately weak positive or even strong negative responses. Vegetation growth in the boreal NH was more vulnerable to extremely high-temperature events than vegetation growth in the temporal NH. The non-linear responses discovered here provide new insights into the dynamics of northern terrestrial ecosystems in a warmer world.

scholarly journals Implementation of a Marauding Insect Module (MIM, version 1.0) in the Integrated BIosphere Simulator (IBIS, version 2.6b4) Dynamic Vegetation–Land Surface Model

2015 ◽  
Vol 8 (12) ◽  
pp. 10365-10409
Author(s):  
J.-S. Landry ◽  
D. T. Price ◽  
N. Ramankutty ◽  
L. Parrott ◽  
H. D. Matthews
Keyword(s):  
Land Surface ◽  
Vegetation Dynamics ◽  
Bark Beetles ◽  
Mountain Pine Beetle ◽  
Land Surface Model ◽  
Field Measurements ◽  
Surface Model ◽  
Climatic Effects ◽  
Standing Trees ◽  
Integrated Biosphere Simulator

Abstract. Insects defoliate and kill plants in many ecosystems worldwide. The consequences of these natural processes on terrestrial ecology and nutrient cycling are well established, and their potential climatic effects resulting from modified land–atmosphere exchanges of carbon, energy, and water are increasingly being recognized. We developed a Marauding Insect Module (MIM) to quantify, in the Integrated BIosphere Simulator (IBIS), the consequences of insect activity on biogeochemical and biogeophysical fluxes, also accounting for the effects of altered vegetation dynamics. MIM can simulate damage from broadleaf defoliators, needleleaf defoliators, and bark beetles, with the resulting impacts being estimated by IBIS based on the new, insect-modified state of the vegetation. MIM further accounts for the physical presence and gradual fall of insect-killed dead standing trees. The design of MIM should facilitate the addition of other insect types besides the ones already included and could guide the development of similar modules for other process-based vegetation models. After describing IBIS-MIM, we illustrate the usefulness of the model by presenting results spanning daily to centennial timescales for vegetation dynamics and cycling of carbon, energy, and water following a simulated outbreak of the mountain pine beetle. We then show that these simulated impacts agree with many previous studies based on field measurements, satellite data, or modelling. MIM and similar tools should therefore be of great value in assessing the wide array of impacts resulting from insect-induced plant damage in the Earth system.

L'apport de la télédétection spatiale à la modélisation des surfaces continentales

2020 ◽  
pp. 052
Author(s):  
Jean-Christophe Calvet ◽  
Jean-Louis Champeaux
Keyword(s):  
Satellite Data ◽  
Land Surface ◽  
Land Surface Model ◽  
Static Model ◽  
Geographic Information ◽  
Surface Model ◽  
Model Parameters

Cet article présente les différentes étapes des développements réalisés au CNRM des années 1990 à nos jours pour spatialiser à diverses échelles les simulations du modèle Isba des surfaces terrestres. Une attention particulière est portée sur l'intégration, dans le modèle, de données satellitaires permettant de caractériser la végétation. Deux façons complémentaires d'introduire de l'information géographique dans Isba sont présentées : cartographie de paramètres statiques et intégration au fil de l'eau dans le modèle de variables observables depuis l'espace. This paper presents successive steps in developments made at CNRM from the 1990s to the present-day in order to spatialize the simulations of the Isba land surface model at various scales. The focus is on the integration in the model of satellite data informative about vegetation. Two complementary ways to integrate geographic information in Isba are presented: mapping of static model parameters and sequential assimilation of variables observable from space.

Sign in / Sign up

Export Citation Format

Share Document