Space and Time Variations in Specifying Monthly Mean Surface Temperature from the 700 mb Height Field

1985 ◽  
Vol 113 (3) ◽  
pp. 277-290 ◽  
Author(s):  
William H. Klein
2021 ◽  
Vol 10 (8) ◽  
pp. 500
Author(s):  
Lianwei Li ◽  
Yangfeng Xu ◽  
Cunjin Xue ◽  
Yuxuan Fu ◽  
Yuanyu Zhang

It is important to consider where, when, and how the evolution of sea surface temperature anomalies (SSTA) plays significant roles in regional or global climate changes. In the comparison of where and when, there is a great challenge in clearly describing how SSTA evolves in space and time. In light of the evolution from generation, through development, and to the dissipation of SSTA, this paper proposes a novel approach to identifying an evolution of SSTA in space and time from a time-series of a raster dataset. This method, called PoAIES, includes three key steps. Firstly, a cluster-based method is enhanced to explore spatiotemporal clusters of SSTA, and each cluster of SSTA at a time snapshot is taken as a snapshot object of SSTA. Secondly, the spatiotemporal topologies of snapshot objects of SSTA at successive time snapshots are used to link snapshot objects of SSTA into an evolution object of SSTA, which is called a process object. Here, a linking threshold is automatically determined according to the overlapped areas of the snapshot objects, and only those snapshot objects that meet the specified linking threshold are linked together into a process object. Thirdly, we use a graph-based model to represent a process object of SSTA. A node represents a snapshot object of SSTA, and an edge represents an evolution between two snapshot objects. Using a number of child nodes from an edge’s parent node and a number of parent nodes from the edge’s child node, a type of edge (an evolution relationship) is identified, which shows its development, splitting, merging, or splitting/merging. Finally, an experiment on a simulated dataset is used to demonstrate the effectiveness and the advantages of PoAIES, and a real dataset of satellite-SSTA is used to verify the rationality of PoAIES with the help of ENSO’s relevant knowledge, which may provide new references for global change research.


1974 ◽  
Vol 36 (11) ◽  
pp. 1841-1849 ◽  
Author(s):  
Yu.D Iljichev ◽  
I.A Lysenko ◽  
A.D Orlyansky ◽  
Yu.I Portnyagin

2016 ◽  
Vol 43 (3) ◽  
pp. 438-447 ◽  
Author(s):  
L. V. Kuksina ◽  
N. I. Alekseevskii

1976 ◽  
Vol 6 (3) ◽  
pp. 247-252 ◽  
Author(s):  
Erwin R. Berglund ◽  
Arnett C. Mace Jr.

Diurnal albedo relationships were determined for black spruce (Piceamariana (Mill.) B.S.P.) and sphagnum–sedge bogs in northern Minnesota. Two opposing, cart-mounted, Kipp and Zonen pyranometers traversed a tramway to integrate space and time variations of incoming and reflected solar radiation (waveband 0.3–3.0 microns (μ)).The black spruce stand's diurnal albedo was parabolic. Albedo increased with solar altitude to a maximum at 1200 h (7–8%) and then decreased. Greatest within-season variation occurred during June and September. Canopy roughness was the dominant influence on albedo variation and differences.The sphagnum–sedge type diurnal albedo was M-shaped. A minimum albedo between two maxima occurred at 1200 h. Albedos increased from the 1200-h minimum to each maxima as a result of reported surface 'flattening' effects, increased specular reflection, and changes in solar radiation quality. Albedos before the first and after the second maxima were dominated by the microrelief roughness of the sphagnum–sedge hummocks.


2020 ◽  
Vol 47 (4) ◽  
pp. 629-640
Author(s):  
N. M. Shesterkina ◽  
V. P. Shesterkin ◽  
V. S. Talovskaya ◽  
T. D. Ri

2016 ◽  
Vol 52 (2) ◽  
pp. 176-187 ◽  
Author(s):  
S. N. Kulichkov ◽  
I. P. Chunchuzov ◽  
G. A. Bush ◽  
A. A. Mishenin ◽  
E. V. Golikova

2021 ◽  
Author(s):  
Ankur R. Desai ◽  
Anam M. Khan ◽  
Ting Zheng ◽  
Sreenath Paleri ◽  
Brian Butterworth ◽  
...  

2019 ◽  
Vol 46 (S1) ◽  
pp. S74-S84 ◽  
Author(s):  
R. G. Dzhamalov ◽  
K. G. Vlasov ◽  
K. G. Myagkova ◽  
O. S. Reshetnyak ◽  
T. I. Safronova

1967 ◽  
Vol 72 (17) ◽  
pp. 4590-4594 ◽  
Author(s):  
F. R. Paolini ◽  
G. C. Theodoridis ◽  
S. Frankenthal

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