Daily variations of temperature and humidity within and above Amazonian forest.

W. James Shuttleworth

Daily variations of temperature and humidity within and above Amazonian forest.

Research output: Contribution to journal › Article › peer-review

Abstract

The behavior of profiles of humidity and temperature above and within the canopy of Amazonian forest in dry and wet conditions is demonstrated; qualitative insight into some of the processes involved in energy exchange from this type of vegetation is allowed. In dry daylight conditions the temperature, humidity and humidity deficit of the top two thirds of the canopy are similar to those of the atmosphere above, but air at the base of the canopy is strongly decoupled. At night the behaviour is reversed, and air in the lower two-thirds of the canopy is partly decoupled from that at higher levels. The response to convective storms is rapid but fairly short lived, and local energy advection can occur during and after rainfall.-from STAR, 22(21), 1984

Original language	English (US)
Journal	[No source information available]
State	Published - Jan 1 1984
Externally published	Yes

ASJC Scopus subject areas

Environmental Science(all)
Earth and Planetary Sciences(all)

Fingerprint Dive into the research topics of 'Daily variations of temperature and humidity within and above Amazonian forest.'. Together they form a unique fingerprint.

Cite this

@article{072faecbfaa94eb6bb638f6eac307e5f,

title = "Daily variations of temperature and humidity within and above Amazonian forest.",

abstract = "The behavior of profiles of humidity and temperature above and within the canopy of Amazonian forest in dry and wet conditions is demonstrated; qualitative insight into some of the processes involved in energy exchange from this type of vegetation is allowed. In dry daylight conditions the temperature, humidity and humidity deficit of the top two thirds of the canopy are similar to those of the atmosphere above, but air at the base of the canopy is strongly decoupled. At night the behaviour is reversed, and air in the lower two-thirds of the canopy is partly decoupled from that at higher levels. The response to convective storms is rapid but fairly short lived, and local energy advection can occur during and after rainfall.-from STAR, 22(21), 1984",

author = "Shuttleworth, {W. James}",

year = "1984",

month = jan,

day = "1",

language = "English (US)",

journal = "[No source information available]",

}

TY - JOUR

T1 - Daily variations of temperature and humidity within and above Amazonian forest.

AU - Shuttleworth, W. James

PY - 1984/1/1

Y1 - 1984/1/1

N2 - The behavior of profiles of humidity and temperature above and within the canopy of Amazonian forest in dry and wet conditions is demonstrated; qualitative insight into some of the processes involved in energy exchange from this type of vegetation is allowed. In dry daylight conditions the temperature, humidity and humidity deficit of the top two thirds of the canopy are similar to those of the atmosphere above, but air at the base of the canopy is strongly decoupled. At night the behaviour is reversed, and air in the lower two-thirds of the canopy is partly decoupled from that at higher levels. The response to convective storms is rapid but fairly short lived, and local energy advection can occur during and after rainfall.-from STAR, 22(21), 1984

AB - The behavior of profiles of humidity and temperature above and within the canopy of Amazonian forest in dry and wet conditions is demonstrated; qualitative insight into some of the processes involved in energy exchange from this type of vegetation is allowed. In dry daylight conditions the temperature, humidity and humidity deficit of the top two thirds of the canopy are similar to those of the atmosphere above, but air at the base of the canopy is strongly decoupled. At night the behaviour is reversed, and air in the lower two-thirds of the canopy is partly decoupled from that at higher levels. The response to convective storms is rapid but fairly short lived, and local energy advection can occur during and after rainfall.-from STAR, 22(21), 1984

UR - http://www.scopus.com/inward/record.url?scp=85040845551&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=85040845551&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:85040845551

JO - [No source information available]

JF - [No source information available]

ER -

Daily variations of temperature and humidity within and above Amazonian forest.

Abstract

ASJC Scopus subject areas

Other files and links

Cite this