Authors |
Safriel U. , Adeel Z. , Niemeijer D. , PuigdefÂbrega J. , White R. , Lal R. , Winslow M. , Ziedler J. , Prince S. , Archer E. , King C. , Shapiro B. , Wessels K.J. , Nielsen T. , Portnov B. , Reshef I. , Thonell J. , Lachman E. , Mcnab D. |
Source |
Island Press (4) |
Type |
C - Chapter (105) |
Peer Review |
2 - Medium (2288) |
Audience |
S - Specialist (3514) |
Pages |
623-662 |
Notes |
Drylands cover about 41% of Earth’s land surface and are inhabited by more than 2 billion people (about one third of world population). Drylands are limited by soil moisture, the result of low rainfall and high evaporation, and show a gradient of increasing primary productivity, ranging from hyper-arid, arid, and semiarid to dry subhumid areas. Deserts, grasslands, and woodlands are the natural expression of this gradient. |
Entered by: Rachel Downey, 4/2009