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Record #112443:
- #112443
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MARC recordAlpine permafrost temperature zonality, northern trans-Baikal region, U.S.S.R. / N.N. Romanovskiy, V.N. Zaitsev, S.Yu. Volchenkoc, D.D. Zagryazkin, D.O. Sergeyev.
| Title: | Alpine permafrost temperature zonality, northern trans-Baikal region, U.S.S.R. / N.N. Romanovskiy, V.N. Zaitsev, S.Yu. Volchenkoc, D.D. Zagryazkin, D.O. Sergeyev. |
| Author(s): | Romanovskiy, N. N. Zaitsev, V. N. Volchenkoc, S. Yu. Zagryazkin, D. D. Sergeyev, D. O. |
| Date: | 1991. |
| In: | Permafrost and Periglacial Processes. (1991.), Vol. 2(3) (1991) |
| Abstract: | New method of data processing used, which involves mean annual ground temperatures at depth of zero annual altitude (tan). Used with results of geocryological survey, mean ground temperature is calculated. Understanding of vertical zonality of permafrost ground temperatures may be derived from change in mean ground temperature with change in altitude, calculated for certain altitudinal intervals; variations in tan for different natural conditions; and range of tan changes, averaged for each landscape type. |
| Notes: | Permafrost and Periglacial Processes. Vol. 2(3) :187-195 (1991). |
| Keywords: | 551.32 -- Glaciology. 551.345 -- Permafrost. Cryopedology. 536 -- Heat. 551.345.2 -- Permafrost, formation and decay. E8 -- Glaciology: frost action and permafrost. (*50) -- Soviet Union. |
| SPRI record no.: | 112443 |
LDR 01575naa#a2200000#a#4500 001 SPRI-112443 005 20230401210154.0 007 ta 008 230401s1991####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-112443 040 ## ‡aUkCU-P‡beng‡eaacr 245 00 ‡aAlpine permafrost temperature zonality, northern trans-Baikal region, U.S.S.R. /‡cN.N. Romanovskiy, V.N. Zaitsev, S.Yu. Volchenkoc, D.D. Zagryazkin, D.O. Sergeyev. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1991. 300 ## ‡ap. 187-195 :‡bdiags., table, map. 500 ## ‡aPermafrost and Periglacial Processes. Vol. 2(3) :187-195 (1991). 520 3# ‡aNew method of data processing used, which involves mean annual ground temperatures at depth of zero annual altitude (tan). Used with results of geocryological survey, mean ground temperature is calculated. Understanding of vertical zonality of permafrost ground temperatures may be derived from change in mean ground temperature with change in altitude, calculated for certain altitudinal intervals; variations in tan for different natural conditions; and range of tan changes, averaged for each landscape type. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.345 -- Permafrost. Cryopedology.‡2udc 650 07 ‡a536 -- Heat.‡2udc 650 07 ‡a551.345.2 -- Permafrost, formation and decay.‡2udc 650 07 ‡aE8 -- Glaciology: frost action and permafrost.‡2local 651 #7 ‡a(*50) -- Soviet Union.‡2udc 700 1# ‡aRomanovskiy, N. N. 700 1# ‡aZaitsev, V. N. 700 1# ‡aVolchenkoc, S. Yu. 700 1# ‡aZagryazkin, D. D. 700 1# ‡aSergeyev, D. O. 773 0# ‡7nnas ‡tPermafrost and Periglacial Processes. ‡gVol. 2(3) (1991) ‡wSPRI-102743 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230401