scholarly journals The Cyclical Behavior of the Price‐Cost Markup

2020 ◽  
Vol 52 (S2) ◽  
pp. 319-353 ◽  
Author(s):  
CHRISTOPHER J. NEKARDA ◽  
VALERIE A. RAMEY
Keyword(s):  
Cyclical Behavior

Cyclical Behavior of Coronal Mass Ejections

Solar Physics ◽  
2009 ◽  
Vol 257 (1) ◽  
pp. 149-154 ◽  
Author(s):  
K. J. Li ◽  
P. X. Gao ◽  
Q. X. Li ◽  
J. Mu ◽  
T. W. Su
Keyword(s):  
Coronal Mass Ejections ◽  
Cyclical Behavior

Using theory for measurement: An analysis of the cyclical behavior of home production

1997 ◽  
Vol 40 (3) ◽  
pp. 435-456 ◽  
Author(s):  
Beth F. Ingram ◽  
Narayana R. Kocherlakota ◽  
N.E. Savin
Keyword(s):  
Home Production ◽  
Cyclical Behavior

scholarly journals A conceptual model of cyclical glacier flow in overdeepenings

2014 ◽  
Vol 8 (4) ◽  
pp. 4463-4495 ◽  
Author(s):  
J. B. Turrin ◽  
R. R. Forster
Keyword(s):  
Conceptual Model ◽  
The Other ◽  
Acceleration Phase ◽  
Alaska Range ◽  
Deceleration Phase ◽  
Surface Slopes ◽  
Glacier Dynamics ◽  
Major Tributary ◽  
Cyclical Behavior ◽  
Glacier Flow

Abstract. A nearly four-decade, satellite-based velocity survey of the largest glaciers in the Alaska Range, Chugach Mountains, and the Wrangell Mountains of southern Alaska, spanning the early- to mid-1970s through the 2000s, reveals nine pulsing glaciers: Capps, Copper, Eldridge, Kahiltna, Matanuska, Nabesna, Nizina, Ruth, and Sanford glaciers. The pulses increase velocity by up to 2449% (Capps Glacier) or as little as 77% (Nabesna Glacier), with velocity increases for the other glaciers in the range of 100–250%. The pulses may last from between six years (Copper Glacier) to 12 years (Nizina Glacier) and consist of a multi-year acceleration phase followed by a multi-year deceleration phase during which significant portions of each glacier move en masse. The segments of each glacier affected by the pulses may be anywhere from 14 km (Sanford Glacier) to 36 km (Nabesna Glacier) in length and occur where the glaciers are either laterally constricted or joined by a major tributary, and the surface slopes at these locations are very shallow, 1–2°, suggesting the pulses occur where the glaciers are overdeepened. A conceptual model to explain the cyclical behavior of these pulsing glaciers is presented that incorporates the effects of glaciohydraulic supercooling, glacier dynamics, surface ablation, and subglacial sediment erosion, deposition, and deformation in overdeepenings.

scholarly journals Major Changes in Cyclical Behavior

10.3386/w1395 ◽  
1984 ◽  
Author(s):  
Victor Zarnowitz ◽  
Geoffrey Moore
Keyword(s):  
Cyclical Behavior
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