dc.creator |
Vergara, Walter |
|
dc.creator |
Scholz, Sebastian M. |
|
dc.date |
2012-03-19T09:35:51Z |
|
dc.date |
2012-03-19T09:35:51Z |
|
dc.date |
2011 |
|
dc.date.accessioned |
2023-02-17T20:37:56Z |
|
dc.date.available |
2023-02-17T20:37:56Z |
|
dc.identifier |
http://www-wds.worldbank.org/external/default/main?menuPK=64187510&pagePK=64193027&piPK=64187937&theSitePK=523679&menuPK=64187510&searchMenuPK=64187283&siteName=WDS&entityID=000333037_20101124000244 |
|
dc.identifier |
978-0-8213-8621-7 |
|
dc.identifier |
http://hdl.handle.net/10986/2531 |
|
dc.identifier.uri |
http://localhost:8080/xmlui/handle/CUHPOERS/242954 |
|
dc.description |
The Amazon basin is a key component of
the global carbon cycle. The old-growth rainforests in the
basin represent storage of ~ 120 petagrams of carbon (Pg C)
in their biomass. Annually, these tropical forests process
approximately 18 Pg C through respiration and
photosynthesis. This is more than twice the rate of global
anthropogenic fossil fuel emissions. The basin is also the
largest global repository of biodiversity and produces about
20 percent of the world's flow of fresh water into the
oceans. Despite the large carbon dioxide (CO2) efflux from
recent deforestation, the Amazon rainforest ecosystem is
still considered to be a net carbon sinks of 0.8-1.1 Pg C
per year because growth on average exceeds mortality
(Phillips et al. 2008). However, current climate trends and
human-induced deforestation may be transforming forest
structure and behavior (Phillips et al. 2009). Increasing
temperatures may accelerate respiration rates and thus
carbon emissions from soils (Malhi and Grace 2000). High
probabilities for modification in rainfall patterns (Malhi
et al. 2008) and prolonged drought stress may lead to
reductions in biomass density. Resulting changes in
evapo-transpiration and therefore convective precipitation
could further accelerate drought conditions and destabilize
the tropical ecosystem as a whole, causing a reduction in
its biomass carrying capacity or dieback. In turn, changes
in the structure of the Amazon and its associated water
cycle will have implications for the many endemic species it
contains and result in changes at a continental scale.
Clearly, with much at stake, if climate-induced damage
alters the state of the Amazon ecosystem, there is a need to
better understand its risk, process, and dynamics. The
objective of this study is to assist in understanding the
risk, process, and dynamics of potential Amazon dieback and
its implications. |
|
dc.language |
English |
|
dc.publisher |
World Bank |
|
dc.relation |
A World Bank study |
|
dc.rights |
CC BY 3.0 IGO |
|
dc.rights |
http://creativecommons.org/licenses/by/3.0/igo |
|
dc.rights |
World Bank |
|
dc.subject |
ABOVEGROUND VEGETATION |
|
dc.subject |
AEROSOLS |
|
dc.subject |
AIR |
|
dc.subject |
AIR TEMPERATURE |
|
dc.subject |
AMAZON DEFORESTATION |
|
dc.subject |
AMAZON FOREST |
|
dc.subject |
AMAZON RAINFOREST |
|
dc.subject |
AMAZONIAN FOREST |
|
dc.subject |
AMAZONIAN RAINFALL |
|
dc.subject |
ANNUAL PRECIPITATION |
|
dc.subject |
ATMOSPHERE |
|
dc.subject |
ATMOSPHERE-OCEAN GENERAL CIRCULATION |
|
dc.subject |
ATMOSPHEREOCEAN GENERAL CIRCULATION |
|
dc.subject |
ATMOSPHERIC CARBON |
|
dc.subject |
ATMOSPHERIC CARBON DIOXIDE |
|
dc.subject |
ATMOSPHERIC RESEARCH |
|
dc.subject |
BIOCLIMATIC LIMITS |
|
dc.subject |
BIOMASS CARBON |
|
dc.subject |
BIOMASS DENSITY |
|
dc.subject |
BIOSPHERE |
|
dc.subject |
CARBON |
|
dc.subject |
CARBON CHANGE |
|
dc.subject |
CARBON CONTENT |
|
dc.subject |
CARBON DIOXIDE LEVELS |
|
dc.subject |
CARBON EMISSION |
|
dc.subject |
CARBON EMISSIONS |
|
dc.subject |
CARBON SINK |
|
dc.subject |
CARBON STARVATION |
|
dc.subject |
CENTURY TEMPERATURE |
|
dc.subject |
CLEAN ENERGY |
|
dc.subject |
CLIMATE |
|
dc.subject |
CLIMATE CHANGE |
|
dc.subject |
CLIMATE CHANGE ADAPTATION |
|
dc.subject |
CLIMATE CHANGE IMPACTS |
|
dc.subject |
CLIMATE CHANGE PROJECTIONS |
|
dc.subject |
CLIMATE CHANGE SCENARIOS |
|
dc.subject |
CLIMATE CHANGES |
|
dc.subject |
CLIMATE CONDITIONS |
|
dc.subject |
CLIMATE EQUILIBRIUM |
|
dc.subject |
CLIMATE EXTREMES |
|
dc.subject |
CLIMATE FEEDBACKS |
|
dc.subject |
CLIMATE FORCING |
|
dc.subject |
CLIMATE IMPACT |
|
dc.subject |
CLIMATE IMPACT RESEARCH |
|
dc.subject |
CLIMATE IMPACTS |
|
dc.subject |
CLIMATE MODEL |
|
dc.subject |
CLIMATE MODELS |
|
dc.subject |
CLIMATE POLICIES |
|
dc.subject |
CLIMATE PREDICTION |
|
dc.subject |
CLIMATE RESEARCH |
|
dc.subject |
CLIMATE RESEARCH UNIT |
|
dc.subject |
CLIMATE SCENARIO |
|
dc.subject |
CLIMATE SCENARIOS |
|
dc.subject |
CLIMATE SCIENCE |
|
dc.subject |
CLIMATE SIMULATION |
|
dc.subject |
CLIMATE SIMULATIONS |
|
dc.subject |
CLIMATE TRENDS |
|
dc.subject |
CLIMATE-VEGETATION MODEL |
|
dc.subject |
CLIMATIC CHANGES |
|
dc.subject |
CLIMATIC CONDITIONS |
|
dc.subject |
CLIMATIC FACTORS |
|
dc.subject |
CLIMATIC RESEARCH |
|
dc.subject |
CLIMATIC VARIABLE |
|
dc.subject |
CLIMATOLOGY |
|
dc.subject |
CLOUD COVER |
|
dc.subject |
CLOUDS |
|
dc.subject |
CO2 |
|
dc.subject |
COLORS |
|
dc.subject |
CONVECTIVE PRECIPITATION |
|
dc.subject |
CONVERGENCE |
|
dc.subject |
CRU |
|
dc.subject |
DEFORESTATION |
|
dc.subject |
DEFORESTATION SCENARIOS |
|
dc.subject |
DROUGHT |
|
dc.subject |
DRY FORESTS |
|
dc.subject |
DRY SEASON |
|
dc.subject |
DYNAMIC GLOBAL VEGETATION MODEL |
|
dc.subject |
ECOSYSTEM |
|
dc.subject |
ECOSYSTEM RESILIENCE |
|
dc.subject |
ECOSYSTEM RESPONSES |
|
dc.subject |
ECOSYSTEM STRUCTURE |
|
dc.subject |
EMISSION |
|
dc.subject |
EMISSION SCENARIO |
|
dc.subject |
EMISSION SCENARIOS |
|
dc.subject |
EMISSION TRAJECTORIES |
|
dc.subject |
EMISSIONS |
|
dc.subject |
EMISSIONS FROM SOILS |
|
dc.subject |
EMISSIONS SCENARIOS |
|
dc.subject |
ENDEMIC SPECIES |
|
dc.subject |
ENERGY EFFICIENCY |
|
dc.subject |
ENVIRONMENTAL CONDITIONS |
|
dc.subject |
ENVIRONMENTAL ECONOMIST |
|
dc.subject |
EVAPORATION |
|
dc.subject |
EVAPOTRANSPIRATION |
|
dc.subject |
EXTREME DRY |
|
dc.subject |
EXTREME EVENTS |
|
dc.subject |
EXTREME PRECIPITATION |
|
dc.subject |
EXTREME PRECIPITATION EVENTS |
|
dc.subject |
EXTREME WEATHER |
|
dc.subject |
EXTREME WEATHER EVENTS |
|
dc.subject |
FERTILIZATION |
|
dc.subject |
FLOODS |
|
dc.subject |
FOREST |
|
dc.subject |
FOREST BIOMASS |
|
dc.subject |
FOREST BIOMASS ESTIMATE |
|
dc.subject |
FOREST CARBON |
|
dc.subject |
FOREST CONSERVATION |
|
dc.subject |
FOREST COVER |
|
dc.subject |
FOREST DEGRADATION |
|
dc.subject |
FOREST DIEBACK |
|
dc.subject |
FOREST ECOSYSTEMS |
|
dc.subject |
FOREST GROWTH |
|
dc.subject |
FOREST MICROCLIMATOLOGY |
|
dc.subject |
FOREST STANDS |
|
dc.subject |
FOREST STRUCTURE |
|
dc.subject |
FOREST TYPES |
|
dc.subject |
FORESTS |
|
dc.subject |
FOSSIL FUEL |
|
dc.subject |
FOSSIL FUEL EMISSIONS |
|
dc.subject |
FOSSIL FUELS |
|
dc.subject |
GCM |
|
dc.subject |
GENERAL CIRCULATION MODEL |
|
dc.subject |
GHG |
|
dc.subject |
GHGS |
|
dc.subject |
GLOBAL AVERAGE SURFACE WARMING |
|
dc.subject |
GLOBAL BIODIVERSITY |
|
dc.subject |
GLOBAL CARBON CYCLE |
|
dc.subject |
GLOBAL CLIMATE |
|
dc.subject |
GLOBAL EMISSION |
|
dc.subject |
GLOBAL EMISSIONS |
|
dc.subject |
GLOBAL GREENHOUSE GAS |
|
dc.subject |
GLOBAL GREENHOUSE GAS EMISSION |
|
dc.subject |
GLOBAL PRECIPITATION |
|
dc.subject |
GLOBAL PRECIPITATION CLIMATOLOGY |
|
dc.subject |
GLOBAL SCALE |
|
dc.subject |
GLOBAL VEGETATION |
|
dc.subject |
GLOBAL WARMING |
|
dc.subject |
GREENHOUSE |
|
dc.subject |
GREENHOUSE GASES |
|
dc.subject |
HYDROLOGICAL CHANGES |
|
dc.subject |
HYDROLOGY |
|
dc.subject |
ICE |
|
dc.subject |
IMPACT OF CLIMATE |
|
dc.subject |
IMPACTS OF CLIMATE CHANGE |
|
dc.subject |
INTERGOVERNMENTAL PANEL ON CLIMATE CHANGE |
|
dc.subject |
INTERNATIONAL CLIMATE POLICY |
|
dc.subject |
INTERTROPICAL CONVERGENCE ZONE |
|
dc.subject |
IPCC |
|
dc.subject |
ITCZ |
|
dc.subject |
LAND SURFACE |
|
dc.subject |
LAND USE |
|
dc.subject |
LAND USE CHANGE |
|
dc.subject |
LAND USE CHANGES |
|
dc.subject |
LIGHTNING |
|
dc.subject |
LOSS OF VEGETATION |
|
dc.subject |
MEAN RAINFALL |
|
dc.subject |
METEOROLOGICAL RESEARCH |
|
dc.subject |
METHANE |
|
dc.subject |
NITROGEN |
|
dc.subject |
OCEANS |
|
dc.subject |
PHOTOSYNTHESIS |
|
dc.subject |
PLANT GROWTH |
|
dc.subject |
PRECIPITATION |
|
dc.subject |
RADIATIVE FORCING |
|
dc.subject |
RAIN |
|
dc.subject |
RAINFALL |
|
dc.subject |
RAINFALL ANOMALIES |
|
dc.subject |
RAINFALL DISTRIBUTIONS |
|
dc.subject |
RAINFALL REDUCTION |
|
dc.subject |
RAINFALL TREND |
|
dc.subject |
RAINFALL VARIABILITY |
|
dc.subject |
RENEWABLE ENERGY |
|
dc.subject |
RESPONSE TO CLIMATE CHANGE |
|
dc.subject |
SCIENTISTS |
|
dc.subject |
SEA LEVEL RISE |
|
dc.subject |
SEASON |
|
dc.subject |
SEASONAL RAINFALL |
|
dc.subject |
SULPHATE |
|
dc.subject |
SURFACE MODEL |
|
dc.subject |
SURFACE PRESSURE |
|
dc.subject |
SURFACE RUNOFF |
|
dc.subject |
SURFACE TEMPERATURE |
|
dc.subject |
SURFACE TEMPERATURE ANOMALIES |
|
dc.subject |
SURFACE TEMPERATURE CHANGE |
|
dc.subject |
SURFACE TEMPERATURES |
|
dc.subject |
SUSTAINABLE DEVELOPMENT |
|
dc.subject |
TEMPERATE FORESTS |
|
dc.subject |
TEMPERATURE ANOMALIES |
|
dc.subject |
TEMPERATURE ANOMALY |
|
dc.subject |
TEMPERATURE CHANGE |
|
dc.subject |
TEMPERATURE CHANGES |
|
dc.subject |
TEMPERATURE INCREASE |
|
dc.subject |
TEMPERATURE INDEXES |
|
dc.subject |
TREE SPECIES |
|
dc.subject |
TROPICAL BROADLEAF EVERGREEN |
|
dc.subject |
TROPICAL FOREST |
|
dc.subject |
TROPICAL FOREST BIOMASS |
|
dc.subject |
TROPICAL FORESTS |
|
dc.subject |
TROPICS |
|
dc.subject |
URBAN AREAS |
|
dc.subject |
VEGETATION CARBON |
|
dc.subject |
VEGETATION CHANGE |
|
dc.subject |
VEGETATION DYNAMICS |
|
dc.subject |
VEGETATION GROWTH |
|
dc.subject |
WATER CYCLE |
|
dc.subject |
WEATHER FORECASTING |
|
dc.subject |
WEATHER PREDICTION |
|
dc.subject |
WET SEASON |
|
dc.subject |
WIND |
|
dc.subject |
WOODLAND |
|
dc.title |
Assessment of the Risk of Amazon Dieback |
|
dc.type |
Publications & Research :: Publication |
|
dc.type |
Publications & Research :: Publication |
|