Table 1 Spatial scales (km) for the annual surface temperature (LST) and precipitation (P) variations in the S-N and W-E directions for the eight ice-core sites.

From: Satellite measurements reveal strong anisotropy in spatial coherence of climate variations over the Tibet Plateau

 

LST

P

 

S-N

W-E

S-N

W-E

Typical scale for the TP

302

480

111

182

Ice-cores sites

Muztagata

5

207

8

8

Guliya

49

196

8

23

Malan

224

58

8

18

Puruogangri

301

645

23

26

Geladaindong

147

234

24

47

Dunde

36

32

115

69

Dasuopu

26

78

47

127

NoijinKangsang

167

371

8

8

  1. The corresponding typical scales for the entire TP are also shown.
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