![Hier klicken, um den Treffer aus der Auswahl zu entfernen](images/unchecked.gif) |
Titel |
’Together we are stronger ?!’ - Competition and synergies between Plant Functional Types in a changing precipitation regime in North Africa |
VerfasserIn |
Vivienne Groner, Martin Claussen, Christian Reick |
Konferenz |
EGU General Assembly 2016
|
Medientyp |
Artikel
|
Sprache |
en
|
Digitales Dokument |
PDF |
Erschienen |
In: GRA - Volume 18 (2016) |
Datensatznummer |
250124789
|
Publikation (Nr.) |
EGU/EGU2016-4278.pdf |
|
|
|
Zusammenfassung |
The timing and abruptness of vegetation decline at the end of the African Humid Period has
been studied and debated by various working groups using a wide range of models and
palaeo-proxy reconstruction approaches. There have been only few studies addressing
the role of plant diversity in this context. We use a Dynamic Global Vegetation
Model to investigate the potential effect of plant diversity on the abruptness of a
vegetation collapse in an changing precipitation regime in North Africa. Ecologists
agree that high biodiversity can have a stabilizing effect on ecosystems, especially
under changing environmental conditions. However, it remains an open question
how well plant diversity is represented in dynamic models that are widely used for
studies on past climate changes and the consequences for ecosystems, and which
competition and synergy effects determine the retreat of vegetation in aridification
scenarios. Could high plant diversity have strengthened the ecosystem, facilitated
plant growth and prevented an abrupt vegetation collapse at the end of the African
Humid Period? Or could strong competition in a diverse environment have increased
ecosystem resilience resulting in an abrupt vegetation collapse instead of a smooth
decline?
We use the Dynamic Global Vegetation Model JSBACH to study the response of
vegetation to a precipitation decline in North Africa. Diversity is represented by a set of Plant
Functional Types (PFTs). To identify the effects emerging from different degrees of diversity,
we perform simulations with different combinations of PFTs, prescribe atmospheric forcing
and neglect feedbacks between land and atmosphere. First analyses show that vegetation
retreats faster than the prescribed linear precipitation decline in all simulations. In
comparison to single-PFT simulations, competition between PFTs limits in multi-PFT
simulations the expansion and persistence of individual PFTs. The replacement of
retreating PFTs by others that grow better under new conditions smooths the decline of
total vegetation cover and buffers fast retreats of individual PFTs before the final
breakdown.
The set of presented simulations provides the baseline for future coupled simulations that
will account for the entire Earth System, including ocean, atmosphere, and land in its
diversity. |
|
|
|
|
|