from Section Four - Case Studies
Published online by Cambridge University Press: 05 June 2016
Introduction
Savannas are biomes with a discontinuous tree layer and a grass understorey. They are generally tropical or sub-tropical with a distinctly seasonal distribution of rainfall. The two major plant functional types (trees and grasses) have contrasting strategies for surviving the dry season and this is reflected in the seasonality of productivity, leaf area index and patterns in water-use. Woody thickening, whereby the standing biomass of trees increases over time, is a globally observed phenomenon which has implications for carbon (C) storage and catchment water balances of savannas.
Key questions addressed in this case study include: How do tree and grass productivities vary at daily, seasonal and inter-annual time-scales? What are the major drivers of variability in C uptake and water-use at a single site and along rainfall gradients? What is causing woody thickening globally?
A range of field based studies at leaf, canopy and plot scales are discussed in this chapter to illustrate the relationships among meteorological variables at hourly, daily, seasonal and inter-annual time-scales. Remotely sensed data are used to examine: (a) the relative importance of various environmental drivers in explaining differences in productivity; and, (b) large spatial and temporal patterns in phenology along an aridity gradient in north Australia.
Variation in soil moisture content and vapour pressure deficit are vitally important as drivers of daily and seasonal patterns of water-use and C fluxes of savannas. Explanations for inter-annual variations in phenological patterns differ according to aridity and the relative dominance of monsoonal versus convective storm rainfall. Productivity of savannas is very strongly influenced by water availability and much of this is related to changes in LAI of the understorey.
What Are Savannas?
Savannas are characterised by: (i) a high degree of predictability in the occurrence of wet and dry seasons (although timing and amount of rainfall can vary and this can have important impacts on savanna function); (ii) moderate to high temperatures; (iii) the coexistence of a tree dominated overstorey and grass dominated understorey; (iv) the occurrence of fire as a frequent disturbance; and, (v) for tropical and sub-tropical savannas, only small variation in day length. This is contrast to Boreal forests Chapter 14), which are characterised by winters of extreme cold and short day length, and arid and semi-arid grasslands (Chapter 15), which are characterised by very low inputs of rain and extreme variability in the timing and amount of rainfall received each year.
To save this book to your Kindle, first ensure no-reply@cambridge.org is added to your Approved Personal Document E-mail List under your Personal Document Settings on the Manage Your Content and Devices page of your Amazon account. Then enter the ‘name’ part of your Kindle email address below. Find out more about saving to your Kindle.
Note you can select to save to either the @free.kindle.com or @kindle.com variations. ‘@free.kindle.com’ emails are free but can only be saved to your device when it is connected to wi-fi. ‘@kindle.com’ emails can be delivered even when you are not connected to wi-fi, but note that service fees apply.
Find out more about the Kindle Personal Document Service.
To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Dropbox.
To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Google Drive.