An energy budget analysis of water use by Saltcedar

1979 ◽  
Vol 15 (6) ◽  
pp. 1589-1592 ◽  
Author(s):  
L. W. Gay ◽  
L. J. Fritschen
Keyword(s):  
Water Use ◽  
Energy Budget ◽  
Budget Analysis

The fluid-roof solar greenhouse: energy budget analysis by simulation

1981 ◽  
Vol 23 ◽  
pp. 61-76 ◽  
Author(s):  
C.H.M. Van Bavel ◽  
J. Damagnez ◽  
E.J. Sadler
Keyword(s):  
Energy Budget ◽  
Budget Analysis ◽  
Solar Greenhouse

Moisture and Energy Budget Perspectives on Summer Drought in North China

2020 ◽  
Vol 33 (23) ◽  
pp. 10149-10167
Author(s):  
Lan Dai ◽  
Jonathon S. Wright ◽  
Rong Fu
Keyword(s):  
Energy Budget ◽  
Large Scale ◽  
North China ◽  
Static Stability ◽  
Summer Drought ◽  
Warm Core ◽  
Budget Analysis ◽  
Moisture Advection ◽  
Upper Level ◽  
Cold Core

AbstractWe investigate the physical processes behind summer drought in North China by evaluating moisture and energy budget diagnostics and linking them to anomalous large-scale circulation patterns. Moisture budget analysis reveals that summer drought in North China was caused dynamically by reduced vertical moisture advection due to anomalous subsidence and reduced horizontal moisture advection due to anomalous northeasterly winds. Energy budget analysis shows that reduced latent heating was balanced dynamically by decreased dry static energy (DSE) divergence in the middle-to-upper troposphere. Linking these results to previous work, we suggest that summer drought in North China was predicated on co-occurrence of the positive phases of the Eurasian (EU) and Pacific–Japan (PJ) teleconnection patterns, potentially modulated by the circumglobal teleconnection (CGT). In the typical case, the negative phase of the CGT intensified the positive EU-related upper-level cyclone. Resulting upper-level cooling and positive surface feedback imposed a cold-core surface anticyclone that weakened with height. By contrast, when the positive phase of the CGT occurred in tandem with the positive EU and PJ patterns, the anticyclone had a warm core and intensified with height. The two cases were unified by strong subsidence but exhibited opposite meridional advection anomalies. In the cold-core cases, meridional moisture inflow was reduced but meridional DSE export was enhanced, further limiting precipitation while maintaining negative thermal anomalies. In the warm-core case, which only occurred once, enhanced meridional inflow of water vapor supplied moisture for sporadic precipitation while reduced meridional DSE export helped to maintain strong static stability.

Energy budget analysis for Poás crater lake: implications for predicting volcanic activity

Nature ◽  
1989 ◽  
Vol 339 (6223) ◽  
pp. 370-373 ◽  
Author(s):  
Geoff Brown ◽  
Hazel Rymer ◽  
John Dowden ◽  
Phiroze Kapadia ◽  
David Stevenson ◽  
...  
Keyword(s):  
Energy Budget ◽  
Volcanic Activity ◽  
Crater Lake ◽  
Budget Analysis

Basic State Energy Budget Analysis for Phases 1, 2 and 3 of GATE

1983 ◽  
Vol 111 (2) ◽  
pp. 359-369 ◽  
Author(s):  
Randy A. Peppler ◽  
Dayton G. Vincent
Keyword(s):  
Energy Budget ◽  
State Energy ◽  
Budget Analysis

scholarly journals Volcano monitoring by microgravity and energy budget analysis

1991 ◽  
Vol 148 (3) ◽  
pp. 585-593 ◽  
Author(s):  
G. C. BROWN ◽  
H. RYMER ◽  
D. STEVENSON
Keyword(s):  
Energy Budget ◽  
Volcano Monitoring ◽  
Budget Analysis
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