118,399 research outputs found
Genesis, Pathways, and Terminations of Intense Global Water Vapor Transport in Association with Large-Scale Climate Patterns
The CONNected objECT (CONNECT) algorithm is applied to global Integrated Water Vapor Transport data from the NASA's Modern-Era Retrospective Analysis for Research and Applications – Version 2 reanalysis product for the period of 1980 to 2016. The algorithm generates life-cycle records in time and space evolving strong vapor transport events. We show five regions, located in the midlatitudes, where events typically exist (off the coast of the southeast United States, eastern China, eastern South America, off the southern tip of South Africa, and in the southeastern Pacific Ocean). Global statistics show distinct genesis and termination regions and global seasonal peak frequency during Northern Hemisphere late fall/winter and Southern Hemisphere winter. In addition, the event frequency and geographical location are shown to be modulated by the Arctic Oscillation, Pacific North American Pattern, and the quasi-biennial oscillation. Moreover, a positive linear trend in the annual number of objects is reported, increasing by 3.58 objects year-over-year
Tropical Atmospheric Circulations: Dynamic Stability and Transitions
In this article, we present a mathematical theory of the Walker circulation
of the large-scale atmosphere over the tropics. This study leads to a new
metastable state oscillation theory for the El Nino Southern Oscillation
(ENSO), a typical inter-annual climate low frequency oscillation. The
mathematical analysis is based on 1) the dynamic transition theory, 2) the
geometric theory of incompressible flows, and 3) the scaling law for proper
effect of the turbulent friction terms, developed recently by the authors
The ENSO Impact on Predicting World Cocoa Prices
Cocoa beans are produced in equatorial and sub-equatorial regions of West Africa, Southeast Asia and South America. These are also the regions most affected by El Nino Southern Oscillation (ENSO) -- a climatic anomaly affecting temperature and precipitation in many parts of the world. Thus, ENSO, has a potential of affecting cocoa production and, subsequently, prices on the world market. This study investigates the benefits of using a measure of ENSO variable in world cocoa price forecasting through the application of a smooth transition autoregression (STAR) modeling framework to monthly data to examine potentially nonlinear dynamics of ENSO and cocoa prices. The results indicate that the nonlinear models appear to outperform linear models in terms of out-of-sample forecasting accuracy. Furthermore, the results of this study indicate evidence of Granger causality between ENSO and cocoa prices.Cocoa Prices, El Nino Southern Oscillation, Out-of-Sample Forecasting, Smooth Transition Autoregression, Demand and Price Analysis, Environmental Economics and Policy, Research Methods/ Statistical Methods, C32, Q11, Q54,
Solar Meridional Flow in the Shallow Interior during the Rising Phase of Cycle 24
Solar subsurface zonal and meridional-flow profiles during the rising phase
of solar cycle 24 are studied using time-distance helioseismology technique.
The faster zonal bands in the torsional-oscillation pattern show strong
hemispheric asymmetries and temporal variations in both width and speed. The
faster band in the northern hemisphere is located closer to the equator than
the band in the southern hemisphere, and migrates past the equator when the
magnetic activity in the southern hemisphere is reaching maximum. The
meridional-flow speed decreases substantially with the increase of magnetic
activity, and the flow profile shows two zonal structures in each hemisphere.
The residual meridional flow, after subtracting a mean meridional-flow profile,
converges toward the activity belts and shows faster and slower bands like the
torsional-oscillation pattern. More interestingly, the meridional-flow speed
above latitude 30 degree shows an anti-correlation with the
poleward-transporting magnetic flux, slower when the following-polarity flux is
transported and faster when the leading-polarity flux is transported. It is
expected that this phenomenon slows the process of magnetic cancellation and
polarity reversal in the high-latitude areas.Comment: Accepted by ApJ Letter
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