Jornada Experimental Range

Location

32° 36' 52.2288" N, 106° 44' 30.4476" W
Brief Site Description: 
Jornada Experimental Range
Detailed Site Description: 

Jornada Basin LTER 

Research Topics:
desertification; nonlinear dynamics; threshold behavior; cross-scale interactions; cascading events; ecosystem indicators and vegetation dynamics; geomorphology and wind; ecohydrology; animal interactions; factors affecting primary production; animal-induced soil disturbances; direct and indirect consumer effects; vertebrate and invertebrate population dynamics; grazing effects on ecosystem structure and function; biodiversity and ecosystem 

Description:
The overall goal of the Jornada Basin LTER (JRN) program is to quantify the key factors and processes that control ecosystem dynamics and biotic patterns in Chihuahuan Desert landscapes. These landscapes are representative of many arid and semiarid ecosystems of the world where dramatic changes in vegetation structure and ecosystem processes have occurred over the past several centuries. These changes in ecosystem state are often interpreted as “desertification”, the broad-scale conversion of perennial grasslands to dominance by xerophytic woody plants and the associated loss of soils and biological resources, including biodiversity. The JRN LTER has been investigating desertification processes since 1982. Significant advances in understanding the causes and consequences of desertification have been made at specific spatial scales and for certain environmental conditions.

History:
The Jornada Basin Long Term Ecological Research Program (JRN LTER) has been investigating desertification processes since 1982. Significant progress has been made in understanding the causes and consequences of desertification, although key questions remain unresolved, including (1) How do we integrate diverse observations about flora, fauna, soils, hydrology, climate, and human populations across spatial and temporal scales to improve our ability to understand current and historic patterns and dynamics? (2) How do processes interact across a range of scales and under different conditions to drive desertification dynamics and constrain the conservation of biological resources? (3) How can we use knowledge of desertification dynamics to more effectively promote the conservation of biological resources and the recovery of grasslands? This integration is the focus of current LTER studies.

Field Site Type: 
TBD
Registration: 
Unregistered
Network(s): 
ARS
LTAR
LTER
NEON
Study Start Date: 
1912
Mean Annual Precipitation: 
240 millimeters / year
Average Annual Temperature: 
17°C
Average Summer Temperature: 
36°C
Average Winter Temperature: 
13°C
Land Cover: 
Shrubland
Agriculture- Pasture
Geology: 
carbonate
other sedimentary
Soil Order: 
Aridisol
Mollisol
Hydrology: Surface water stream order: 
Unknown
Hydrology: Surface water - Stream Flow Performance: 
Unknown
Hydrology: Groundwater: 
Arrangment of Aquifer Components - Complexly interbedded sequence of aquifers and confining beds
Climate: 
Temperate
Sub-Climate: 
Semiarid
Group visibility: 
Public - accessible to all site users