Chapter 8 The Status and Role of the alpine Cryosphere in Central Asia
The alpine cryosphere including snow, glaciers and permafrost are critical to water management in the Aral Sea Basin (ASB) and larger Central Asia (CA) under changing climate: as they store large amounts of water in its solid forms. Most cryospheric components in the Aral Sea Basin are close to mel...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Hoelzle, Martin [verfasserIn] Barandun, Martina [verfasserIn] Bolch, Tobias [verfasserIn] Fiddes, Joel [verfasserIn] Gafurov, Abror [verfasserIn] Muccione, Veruska [verfasserIn] Saks, Tomas [verfasserIn] Shahgedanova, Maria [verfasserIn] Smakhtin, Vladimir [herausgeberIn] |
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| Format: |
E-Book |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
Erscheinungsort nicht ermittelbar: Taylor & Francis ; 2019 |
|---|
| Rechteinformationen: |
Open Access Creative Commons ; by-nc-nd/4.0 |
|---|
| Schlagwörter: |
|---|
| Umfang: |
1 Online-Ressource (23 p.) |
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| Links: | |
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| ISBN: |
978-0-429-43647-5 |
| Katalog-ID: |
1778511163 |
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| 520 | |a The alpine cryosphere including snow, glaciers and permafrost are critical to water management in the Aral Sea Basin (ASB) and larger Central Asia (CA) under changing climate: as they store large amounts of water in its solid forms. Most cryospheric components in the Aral Sea Basin are close to melting point, and hence very vulnerable to a slight increase in air temperature with significant consequences to long-term water availability and to water resources variability and extremes. Current knowledge about different components of cryosphere and their connection to climate in the Basin and in the entire Central Asia, varies. While it is advanced in the topics of snow and glaciers, knowledge on permafrost it rather limited. Observed trends in runoff point in the direction of increasing water availability in July and August at least until mid-century and increasing possibility for water storage in reservoirs and aquifers. However, eventually this will change as glaciers waste away. Future runoff may change considerably after mid-century and start to decline if not compensated by increasing precipitation. Cryosphere monitoring systems are the basis for sound estimates of water availability and water-related hazards associated with snow, glaciers and permafrost. They require a well-distributed observational network for all cryospheric variables. Such systems need to be re-established in the Basin after the breakup of the Soviet Union in the early 1990s. This process is slowly emerging in the region. Collaboration between local operational hydro-meteorological services and academic sector, and with international research networks may improving the observing capabilities in high mountain regions of CA Asia in general and the ASB specifically | ||
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9780429436475 978-0-429-43647-5 20.500.12854/32828 hdl (DE-627)1778511163 (DE-599)KEP069388636 (OCoLC)1193040949 (DOAB)32828 (EBP)069388636 DE-627 ger DE-627 rakwb eng RBK bicssc RGC bicssc RNC bicssc TQ bicssc Hoelzle, Martin verfasserin aut Chapter 8 The Status and Role of the alpine Cryosphere in Central Asia [Erscheinungsort nicht ermittelbar] Taylor & Francis 2019 1 Online-Ressource (23 p.) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Open Access Unrestricted online access star The alpine cryosphere including snow, glaciers and permafrost are critical to water management in the Aral Sea Basin (ASB) and larger Central Asia (CA) under changing climate: as they store large amounts of water in its solid forms. Most cryospheric components in the Aral Sea Basin are close to melting point, and hence very vulnerable to a slight increase in air temperature with significant consequences to long-term water availability and to water resources variability and extremes. Current knowledge about different components of cryosphere and their connection to climate in the Basin and in the entire Central Asia, varies. While it is advanced in the topics of snow and glaciers, knowledge on permafrost it rather limited. Observed trends in runoff point in the direction of increasing water availability in July and August at least until mid-century and increasing possibility for water storage in reservoirs and aquifers. However, eventually this will change as glaciers waste away. Future runoff may change considerably after mid-century and start to decline if not compensated by increasing precipitation. Cryosphere monitoring systems are the basis for sound estimates of water availability and water-related hazards associated with snow, glaciers and permafrost. They require a well-distributed observational network for all cryospheric variables. Such systems need to be re-established in the Basin after the breakup of the Soviet Union in the early 1990s. This process is slowly emerging in the region. Collaboration between local operational hydro-meteorological services and academic sector, and with international research networks may improving the observing capabilities in high mountain regions of CA Asia in general and the ASB specifically Creative Commons by-nc-nd/4.0 cc English Hydrology & the hydrosphere Human geography Applied ecology Environmental science, engineering & technology Barandun, Martina verfasserin aut Bolch, Tobias verfasserin aut Fiddes, Joel verfasserin aut Gafurov, Abror verfasserin aut Muccione, Veruska verfasserin aut Saks, Tomas verfasserin aut Shahgedanova, Maria verfasserin aut Smakhtin, Vladimir herausgeberin edt https://directory.doabooks.org/handle/20.500.12854/32828 X:DOAB Verlag teilw. kostenfrei ZDB-94-OAB GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_24 ISIL_DE-8 GBV_ILN_30 ISIL_DE-104 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_72 ISIL_DE-35 GBV_ILN_90 ISIL_DE-Hil2 GBV_ILN_91 ISIL_DE-HIL3 GBV_ILN_92 ISIL_DE-33 GBV_ILN_95 ISIL_DE-542 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_130 ISIL_DE-700 GBV_ILN_131 ISIL_DE-Va1 GBV_ILN_136 ISIL_DE-Wis1 GBV_ILN_161 ISIL_DE-960 GBV_ILN_213 ISIL_DE-551 GBV_ILN_230 ISIL_DE-552 GBV_ILN_283 ISIL_DE-Ha163 GBV_ILN_285 ISIL_DE-517 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_635 ISIL_DE-B2138 GBV_ILN_808 GBV_ILN_2011 ISIL_DE-16 GBV_ILN_2018 ISIL_DE-31 GBV_ILN_2034 ISIL_DE-Rt2 GBV_ILN_2037 ISIL_DE-747 GBV_ILN_2050 ISIL_DE-Zi4 GBV_ILN_2108 ISIL_DE-991 BO 20 01 0084 4012036963 OLR-DOAB z 01-12-21 22 01 0018 4006127898 OLR-ZDB-94-OAB DOAB Directory of Open Access Books zu 25-11-21 23 01 0830 4006646275 olr-doab f z 25-11-21 24 01 0008 4060128872 OLR-doab z 15-02-22 30 01 0104 4584174075 OLR-OAB Open Access, Directory of Open Access Books (DOAB) z 28-09-24 60 01 0705 4275956613 OPENAccess Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. Nur für Angehörige der HSU: Volltextzugang von außerhalb des Campus mit Anmeldung über Shibboleth mit Ihrer Bibliothekskennung z 24-02-23 63 01 3401 4106581825 E-Books LF GBV-DOAB z 30-03-22 72 01 0035 4104579920 OLR-ZDB-94-OAB DOAB Directory of Open Access Books z 28-03-22 90 01 3090 4106373564 OLR-HILoapen z 29-03-22 91 01 3091 4011353450 OLR-DOAB DOAB Directory of Open Access Books z 01-12-21 92 01 0033 4110730058 OLR-Open Access DOAB Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. Das Ebook ist frei zugänglich. z 02-04-22 95 01 3095 4342224593 OLR-OAB Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. z 23-06-23 105 01 0841 4007106673 OLR-OAB Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. z 25-11-21 110 01 3110 4584412642 OLR-DOAB Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. Open Access z 28-09-24 130 01 0700 4145767950 OLR-DOAB z 08-06-22 131 01 3131 4465754078 OLR-OA-DOAB Bitte beachten Sie die Nutzungsbedingungen und Copyright-Bestimmungen des Verlages/Herausgebers. z 23-01-24 136 01 3526 4005670598 OLR-DOAB z 24-11-21 161 01 0960 4150912017 OLR-DOAB DOAB Directory of Open Access Books z 16-06-22 213 01 0551 4108551095 OLR-DOAB DOAB Directory of Open Access Books z 31-03-22 230 01 0552 4123489311 OLR-DOAB DOAB Directory of Open Access Books z 27-04-22 283 01 3283 4157068017 Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. z 28-06-22 285 01 0517 4050295776 OLR-DOAB z 03-02-22 293 01 3293 4153708879 OLR-DOAB DOAB Directory of Open Access Books z 21-06-22 370 01 4370 412556289X OLR-FREE Kostenloser Zugriff z 28-04-22 635 01 3635 4509870965 OLR-DOAB Open Access. Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. z 10-04-24 808 01 4808 4158104750 OLR-DOAB DOAB Directory of Open Access Books zg 29-06-22 2011 01 DE-16 4025455676 00 --%%-- --%%-- --%%-- --%%-- l01 22-12-21 2018 01 DE-31 4033386645 00 --%%-- --%%-- --%%-- n Der Zugriff ist kostenfrei möglich. l01 11-01-22 2034 01 DE-Rt2 4014392538 00 --%%-- eBook n n frei zugänglich l01 05-12-21 2037 01 DE-747 434562469X 00 --%%-- eBook OAPEN Foundation OpenAccess --%%-- n Im Internet frei verfügbar l01 30-06-23 2050 01 DE-Zi4 4091562442 00 --%%-- --%%-- --%%-- n Elektronischer Volltext - Open Access l01 16-03-22 2108 01 DE-991 4096793248 00 --%%-- eBook DOAB --%%-- n Elektronischer Volltext - Campuslizenz l01 20-03-22 20 01 0084 https://directory.doabooks.org/handle/20.500.12854/32828 22 01 0018 Volltextzugang https://directory.doabooks.org/handle/20.500.12854/32828 23 01 0830 https://directory.doabooks.org/handle/20.500.12854/32828 24 01 0008 https://directory.doabooks.org/handle/20.500.12854/32828 30 01 0104 https://directory.doabooks.org/handle/20.500.12854/32828 60 01 0705 https://directory.doabooks.org/handle/20.500.12854/32828 63 01 3401 E-Book https://directory.doabooks.org/handle/20.500.12854/32828 72 01 0035 https://directory.doabooks.org/handle/20.500.12854/32828 90 01 3090 https://directory.doabooks.org/handle/20.500.12854/32828 91 01 3091 https://directory.doabooks.org/handle/20.500.12854/32828 92 01 0033 https://directory.doabooks.org/handle/20.500.12854/32828 95 01 3095 https://directory.doabooks.org/handle/20.500.12854/32828 105 01 0841 https://directory.doabooks.org/handle/20.500.12854/32828 110 01 3110 Open Access https://directory.doabooks.org/handle/20.500.12854/32828 130 01 0700 Open Access https://directory.doabooks.org/handle/20.500.12854/32828 131 01 3131 https://directory.doabooks.org/handle/20.500.12854/32828 136 01 3526 Open Access https://directory.doabooks.org/handle/20.500.12854/32828 161 01 0960 https://directory.doabooks.org/handle/20.500.12854/32828 LF 213 01 0551 https://directory.doabooks.org/handle/20.500.12854/32828 230 01 0552 https://directory.doabooks.org/handle/20.500.12854/32828 283 01 3283 https://directory.doabooks.org/handle/20.500.12854/32828 285 01 0517 Open Access https://directory.doabooks.org/handle/20.500.12854/32828 293 01 3293 https://directory.doabooks.org/handle/20.500.12854/32828 LF 370 01 4370 https://directory.doabooks.org/handle/20.500.12854/32828 635 01 3635 https://directory.doabooks.org/handle/20.500.12854/32828 808 01 4808 Volltextzugang https://directory.doabooks.org/handle/20.500.12854/32828 2011 01 DE-16 https://directory.doabooks.org/handle/20.500.12854/32828 2034 01 DE-Rt2 https://directory.doabooks.org/handle/20.500.12854/32828 2037 01 DE-747 https://directory.doabooks.org/handle/20.500.12854/32828 2050 01 DE-Zi4 https://directory.doabooks.org/handle/20.500.12854/32828 2108 01 DE-991 https://directory.doabooks.org/handle/20.500.12854/32828 20 01 0084 OLR-DOAB 22 01 0018 OLR-ZDB-94-OAB 23 01 0830 olr-doab 24 01 0008 OLR-doab 24 01 0008 olr-frei 30 01 0104 OLR-OAB 60 01 0705 OPENAccess 63 01 3401 E-Books LF GBV-DOAB 72 01 0035 OLR-ZDB-94-OAB 90 01 3090 OLR-HILoapen 91 01 3091 OLR-DOAB 92 01 0033 OLR-Open Access DOAB 95 01 3095 OLR-OAB 105 01 0841 OLR-OAB 110 01 3110 OLR-DOAB 130 01 0700 OLR-DOAB 131 01 3131 OLR-OA-DOAB 136 01 3526 OLR-DOAB 161 01 0960 OLR-DOAB 213 01 0551 OLR-DOAB 230 01 0552 OLR-DOAB 285 01 0517 OLR-DOAB 293 01 3293 OLR-DOAB 370 01 4370 OLR-FREE 370 01 4370 olr-ebook ZDB-94-OAB 635 01 3635 OLR-DOAB 808 01 4808 OLR-DOAB |
| spelling |
9780429436475 978-0-429-43647-5 20.500.12854/32828 hdl (DE-627)1778511163 (DE-599)KEP069388636 (OCoLC)1193040949 (DOAB)32828 (EBP)069388636 DE-627 ger DE-627 rakwb eng RBK bicssc RGC bicssc RNC bicssc TQ bicssc Hoelzle, Martin verfasserin aut Chapter 8 The Status and Role of the alpine Cryosphere in Central Asia [Erscheinungsort nicht ermittelbar] Taylor & Francis 2019 1 Online-Ressource (23 p.) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Open Access Unrestricted online access star The alpine cryosphere including snow, glaciers and permafrost are critical to water management in the Aral Sea Basin (ASB) and larger Central Asia (CA) under changing climate: as they store large amounts of water in its solid forms. Most cryospheric components in the Aral Sea Basin are close to melting point, and hence very vulnerable to a slight increase in air temperature with significant consequences to long-term water availability and to water resources variability and extremes. Current knowledge about different components of cryosphere and their connection to climate in the Basin and in the entire Central Asia, varies. While it is advanced in the topics of snow and glaciers, knowledge on permafrost it rather limited. Observed trends in runoff point in the direction of increasing water availability in July and August at least until mid-century and increasing possibility for water storage in reservoirs and aquifers. However, eventually this will change as glaciers waste away. Future runoff may change considerably after mid-century and start to decline if not compensated by increasing precipitation. Cryosphere monitoring systems are the basis for sound estimates of water availability and water-related hazards associated with snow, glaciers and permafrost. They require a well-distributed observational network for all cryospheric variables. Such systems need to be re-established in the Basin after the breakup of the Soviet Union in the early 1990s. This process is slowly emerging in the region. Collaboration between local operational hydro-meteorological services and academic sector, and with international research networks may improving the observing capabilities in high mountain regions of CA Asia in general and the ASB specifically Creative Commons by-nc-nd/4.0 cc English Hydrology & the hydrosphere Human geography Applied ecology Environmental science, engineering & technology Barandun, Martina verfasserin aut Bolch, Tobias verfasserin aut Fiddes, Joel verfasserin aut Gafurov, Abror verfasserin aut Muccione, Veruska verfasserin aut Saks, Tomas verfasserin aut Shahgedanova, Maria verfasserin aut Smakhtin, Vladimir herausgeberin edt https://directory.doabooks.org/handle/20.500.12854/32828 X:DOAB Verlag teilw. kostenfrei ZDB-94-OAB GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_24 ISIL_DE-8 GBV_ILN_30 ISIL_DE-104 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_72 ISIL_DE-35 GBV_ILN_90 ISIL_DE-Hil2 GBV_ILN_91 ISIL_DE-HIL3 GBV_ILN_92 ISIL_DE-33 GBV_ILN_95 ISIL_DE-542 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_130 ISIL_DE-700 GBV_ILN_131 ISIL_DE-Va1 GBV_ILN_136 ISIL_DE-Wis1 GBV_ILN_161 ISIL_DE-960 GBV_ILN_213 ISIL_DE-551 GBV_ILN_230 ISIL_DE-552 GBV_ILN_283 ISIL_DE-Ha163 GBV_ILN_285 ISIL_DE-517 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_635 ISIL_DE-B2138 GBV_ILN_808 GBV_ILN_2011 ISIL_DE-16 GBV_ILN_2018 ISIL_DE-31 GBV_ILN_2034 ISIL_DE-Rt2 GBV_ILN_2037 ISIL_DE-747 GBV_ILN_2050 ISIL_DE-Zi4 GBV_ILN_2108 ISIL_DE-991 BO 20 01 0084 4012036963 OLR-DOAB z 01-12-21 22 01 0018 4006127898 OLR-ZDB-94-OAB DOAB Directory of Open Access Books zu 25-11-21 23 01 0830 4006646275 olr-doab f z 25-11-21 24 01 0008 4060128872 OLR-doab z 15-02-22 30 01 0104 4584174075 OLR-OAB Open Access, Directory of Open Access Books (DOAB) z 28-09-24 60 01 0705 4275956613 OPENAccess Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. Nur für Angehörige der HSU: Volltextzugang von außerhalb des Campus mit Anmeldung über Shibboleth mit Ihrer Bibliothekskennung z 24-02-23 63 01 3401 4106581825 E-Books LF GBV-DOAB z 30-03-22 72 01 0035 4104579920 OLR-ZDB-94-OAB DOAB Directory of Open Access Books z 28-03-22 90 01 3090 4106373564 OLR-HILoapen z 29-03-22 91 01 3091 4011353450 OLR-DOAB DOAB Directory of Open Access Books z 01-12-21 92 01 0033 4110730058 OLR-Open Access DOAB Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. Das Ebook ist frei zugänglich. z 02-04-22 95 01 3095 4342224593 OLR-OAB Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. z 23-06-23 105 01 0841 4007106673 OLR-OAB Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. z 25-11-21 110 01 3110 4584412642 OLR-DOAB Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. Open Access z 28-09-24 130 01 0700 4145767950 OLR-DOAB z 08-06-22 131 01 3131 4465754078 OLR-OA-DOAB Bitte beachten Sie die Nutzungsbedingungen und Copyright-Bestimmungen des Verlages/Herausgebers. z 23-01-24 136 01 3526 4005670598 OLR-DOAB z 24-11-21 161 01 0960 4150912017 OLR-DOAB DOAB Directory of Open Access Books z 16-06-22 213 01 0551 4108551095 OLR-DOAB DOAB Directory of Open Access Books z 31-03-22 230 01 0552 4123489311 OLR-DOAB DOAB Directory of Open Access Books z 27-04-22 283 01 3283 4157068017 Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. z 28-06-22 285 01 0517 4050295776 OLR-DOAB z 03-02-22 293 01 3293 4153708879 OLR-DOAB DOAB Directory of Open Access Books z 21-06-22 370 01 4370 412556289X OLR-FREE Kostenloser Zugriff z 28-04-22 635 01 3635 4509870965 OLR-DOAB Open Access. Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. z 10-04-24 808 01 4808 4158104750 OLR-DOAB DOAB Directory of Open Access Books zg 29-06-22 2011 01 DE-16 4025455676 00 --%%-- --%%-- --%%-- --%%-- l01 22-12-21 2018 01 DE-31 4033386645 00 --%%-- --%%-- --%%-- n Der Zugriff ist kostenfrei möglich. l01 11-01-22 2034 01 DE-Rt2 4014392538 00 --%%-- eBook n n frei zugänglich l01 05-12-21 2037 01 DE-747 434562469X 00 --%%-- eBook OAPEN Foundation OpenAccess --%%-- n Im Internet frei verfügbar l01 30-06-23 2050 01 DE-Zi4 4091562442 00 --%%-- --%%-- --%%-- n Elektronischer Volltext - Open Access l01 16-03-22 2108 01 DE-991 4096793248 00 --%%-- eBook DOAB --%%-- n Elektronischer Volltext - Campuslizenz l01 20-03-22 20 01 0084 https://directory.doabooks.org/handle/20.500.12854/32828 22 01 0018 Volltextzugang https://directory.doabooks.org/handle/20.500.12854/32828 23 01 0830 https://directory.doabooks.org/handle/20.500.12854/32828 24 01 0008 https://directory.doabooks.org/handle/20.500.12854/32828 30 01 0104 https://directory.doabooks.org/handle/20.500.12854/32828 60 01 0705 https://directory.doabooks.org/handle/20.500.12854/32828 63 01 3401 E-Book https://directory.doabooks.org/handle/20.500.12854/32828 72 01 0035 https://directory.doabooks.org/handle/20.500.12854/32828 90 01 3090 https://directory.doabooks.org/handle/20.500.12854/32828 91 01 3091 https://directory.doabooks.org/handle/20.500.12854/32828 92 01 0033 https://directory.doabooks.org/handle/20.500.12854/32828 95 01 3095 https://directory.doabooks.org/handle/20.500.12854/32828 105 01 0841 https://directory.doabooks.org/handle/20.500.12854/32828 110 01 3110 Open Access https://directory.doabooks.org/handle/20.500.12854/32828 130 01 0700 Open Access https://directory.doabooks.org/handle/20.500.12854/32828 131 01 3131 https://directory.doabooks.org/handle/20.500.12854/32828 136 01 3526 Open Access https://directory.doabooks.org/handle/20.500.12854/32828 161 01 0960 https://directory.doabooks.org/handle/20.500.12854/32828 LF 213 01 0551 https://directory.doabooks.org/handle/20.500.12854/32828 230 01 0552 https://directory.doabooks.org/handle/20.500.12854/32828 283 01 3283 https://directory.doabooks.org/handle/20.500.12854/32828 285 01 0517 Open Access https://directory.doabooks.org/handle/20.500.12854/32828 293 01 3293 https://directory.doabooks.org/handle/20.500.12854/32828 LF 370 01 4370 https://directory.doabooks.org/handle/20.500.12854/32828 635 01 3635 https://directory.doabooks.org/handle/20.500.12854/32828 808 01 4808 Volltextzugang https://directory.doabooks.org/handle/20.500.12854/32828 2011 01 DE-16 https://directory.doabooks.org/handle/20.500.12854/32828 2034 01 DE-Rt2 https://directory.doabooks.org/handle/20.500.12854/32828 2037 01 DE-747 https://directory.doabooks.org/handle/20.500.12854/32828 2050 01 DE-Zi4 https://directory.doabooks.org/handle/20.500.12854/32828 2108 01 DE-991 https://directory.doabooks.org/handle/20.500.12854/32828 20 01 0084 OLR-DOAB 22 01 0018 OLR-ZDB-94-OAB 23 01 0830 olr-doab 24 01 0008 OLR-doab 24 01 0008 olr-frei 30 01 0104 OLR-OAB 60 01 0705 OPENAccess 63 01 3401 E-Books LF GBV-DOAB 72 01 0035 OLR-ZDB-94-OAB 90 01 3090 OLR-HILoapen 91 01 3091 OLR-DOAB 92 01 0033 OLR-Open Access DOAB 95 01 3095 OLR-OAB 105 01 0841 OLR-OAB 110 01 3110 OLR-DOAB 130 01 0700 OLR-DOAB 131 01 3131 OLR-OA-DOAB 136 01 3526 OLR-DOAB 161 01 0960 OLR-DOAB 213 01 0551 OLR-DOAB 230 01 0552 OLR-DOAB 285 01 0517 OLR-DOAB 293 01 3293 OLR-DOAB 370 01 4370 OLR-FREE 370 01 4370 olr-ebook ZDB-94-OAB 635 01 3635 OLR-DOAB 808 01 4808 OLR-DOAB |
| allfields_unstemmed |
9780429436475 978-0-429-43647-5 20.500.12854/32828 hdl (DE-627)1778511163 (DE-599)KEP069388636 (OCoLC)1193040949 (DOAB)32828 (EBP)069388636 DE-627 ger DE-627 rakwb eng RBK bicssc RGC bicssc RNC bicssc TQ bicssc Hoelzle, Martin verfasserin aut Chapter 8 The Status and Role of the alpine Cryosphere in Central Asia [Erscheinungsort nicht ermittelbar] Taylor & Francis 2019 1 Online-Ressource (23 p.) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Open Access Unrestricted online access star The alpine cryosphere including snow, glaciers and permafrost are critical to water management in the Aral Sea Basin (ASB) and larger Central Asia (CA) under changing climate: as they store large amounts of water in its solid forms. Most cryospheric components in the Aral Sea Basin are close to melting point, and hence very vulnerable to a slight increase in air temperature with significant consequences to long-term water availability and to water resources variability and extremes. Current knowledge about different components of cryosphere and their connection to climate in the Basin and in the entire Central Asia, varies. While it is advanced in the topics of snow and glaciers, knowledge on permafrost it rather limited. Observed trends in runoff point in the direction of increasing water availability in July and August at least until mid-century and increasing possibility for water storage in reservoirs and aquifers. However, eventually this will change as glaciers waste away. Future runoff may change considerably after mid-century and start to decline if not compensated by increasing precipitation. Cryosphere monitoring systems are the basis for sound estimates of water availability and water-related hazards associated with snow, glaciers and permafrost. They require a well-distributed observational network for all cryospheric variables. Such systems need to be re-established in the Basin after the breakup of the Soviet Union in the early 1990s. This process is slowly emerging in the region. Collaboration between local operational hydro-meteorological services and academic sector, and with international research networks may improving the observing capabilities in high mountain regions of CA Asia in general and the ASB specifically Creative Commons by-nc-nd/4.0 cc English Hydrology & the hydrosphere Human geography Applied ecology Environmental science, engineering & technology Barandun, Martina verfasserin aut Bolch, Tobias verfasserin aut Fiddes, Joel verfasserin aut Gafurov, Abror verfasserin aut Muccione, Veruska verfasserin aut Saks, Tomas verfasserin aut Shahgedanova, Maria verfasserin aut Smakhtin, Vladimir herausgeberin edt https://directory.doabooks.org/handle/20.500.12854/32828 X:DOAB Verlag teilw. kostenfrei ZDB-94-OAB GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_24 ISIL_DE-8 GBV_ILN_30 ISIL_DE-104 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_72 ISIL_DE-35 GBV_ILN_90 ISIL_DE-Hil2 GBV_ILN_91 ISIL_DE-HIL3 GBV_ILN_92 ISIL_DE-33 GBV_ILN_95 ISIL_DE-542 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_130 ISIL_DE-700 GBV_ILN_131 ISIL_DE-Va1 GBV_ILN_136 ISIL_DE-Wis1 GBV_ILN_161 ISIL_DE-960 GBV_ILN_213 ISIL_DE-551 GBV_ILN_230 ISIL_DE-552 GBV_ILN_283 ISIL_DE-Ha163 GBV_ILN_285 ISIL_DE-517 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_635 ISIL_DE-B2138 GBV_ILN_808 GBV_ILN_2011 ISIL_DE-16 GBV_ILN_2018 ISIL_DE-31 GBV_ILN_2034 ISIL_DE-Rt2 GBV_ILN_2037 ISIL_DE-747 GBV_ILN_2050 ISIL_DE-Zi4 GBV_ILN_2108 ISIL_DE-991 BO 20 01 0084 4012036963 OLR-DOAB z 01-12-21 22 01 0018 4006127898 OLR-ZDB-94-OAB DOAB Directory of Open Access Books zu 25-11-21 23 01 0830 4006646275 olr-doab f z 25-11-21 24 01 0008 4060128872 OLR-doab z 15-02-22 30 01 0104 4584174075 OLR-OAB Open Access, Directory of Open Access Books (DOAB) z 28-09-24 60 01 0705 4275956613 OPENAccess Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. Nur für Angehörige der HSU: Volltextzugang von außerhalb des Campus mit Anmeldung über Shibboleth mit Ihrer Bibliothekskennung z 24-02-23 63 01 3401 4106581825 E-Books LF GBV-DOAB z 30-03-22 72 01 0035 4104579920 OLR-ZDB-94-OAB DOAB Directory of Open Access Books z 28-03-22 90 01 3090 4106373564 OLR-HILoapen z 29-03-22 91 01 3091 4011353450 OLR-DOAB DOAB Directory of Open Access Books z 01-12-21 92 01 0033 4110730058 OLR-Open Access DOAB Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. Das Ebook ist frei zugänglich. z 02-04-22 95 01 3095 4342224593 OLR-OAB Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. z 23-06-23 105 01 0841 4007106673 OLR-OAB Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. z 25-11-21 110 01 3110 4584412642 OLR-DOAB Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. Open Access z 28-09-24 130 01 0700 4145767950 OLR-DOAB z 08-06-22 131 01 3131 4465754078 OLR-OA-DOAB Bitte beachten Sie die Nutzungsbedingungen und Copyright-Bestimmungen des Verlages/Herausgebers. z 23-01-24 136 01 3526 4005670598 OLR-DOAB z 24-11-21 161 01 0960 4150912017 OLR-DOAB DOAB Directory of Open Access Books z 16-06-22 213 01 0551 4108551095 OLR-DOAB DOAB Directory of Open Access Books z 31-03-22 230 01 0552 4123489311 OLR-DOAB DOAB Directory of Open Access Books z 27-04-22 283 01 3283 4157068017 Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. z 28-06-22 285 01 0517 4050295776 OLR-DOAB z 03-02-22 293 01 3293 4153708879 OLR-DOAB DOAB Directory of Open Access Books z 21-06-22 370 01 4370 412556289X OLR-FREE Kostenloser Zugriff z 28-04-22 635 01 3635 4509870965 OLR-DOAB Open Access. Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. z 10-04-24 808 01 4808 4158104750 OLR-DOAB DOAB Directory of Open Access Books zg 29-06-22 2011 01 DE-16 4025455676 00 --%%-- --%%-- --%%-- --%%-- l01 22-12-21 2018 01 DE-31 4033386645 00 --%%-- --%%-- --%%-- n Der Zugriff ist kostenfrei möglich. l01 11-01-22 2034 01 DE-Rt2 4014392538 00 --%%-- eBook n n frei zugänglich l01 05-12-21 2037 01 DE-747 434562469X 00 --%%-- eBook OAPEN Foundation OpenAccess --%%-- n Im Internet frei verfügbar l01 30-06-23 2050 01 DE-Zi4 4091562442 00 --%%-- --%%-- --%%-- n Elektronischer Volltext - Open Access l01 16-03-22 2108 01 DE-991 4096793248 00 --%%-- eBook DOAB --%%-- n Elektronischer Volltext - Campuslizenz l01 20-03-22 20 01 0084 https://directory.doabooks.org/handle/20.500.12854/32828 22 01 0018 Volltextzugang https://directory.doabooks.org/handle/20.500.12854/32828 23 01 0830 https://directory.doabooks.org/handle/20.500.12854/32828 24 01 0008 https://directory.doabooks.org/handle/20.500.12854/32828 30 01 0104 https://directory.doabooks.org/handle/20.500.12854/32828 60 01 0705 https://directory.doabooks.org/handle/20.500.12854/32828 63 01 3401 E-Book https://directory.doabooks.org/handle/20.500.12854/32828 72 01 0035 https://directory.doabooks.org/handle/20.500.12854/32828 90 01 3090 https://directory.doabooks.org/handle/20.500.12854/32828 91 01 3091 https://directory.doabooks.org/handle/20.500.12854/32828 92 01 0033 https://directory.doabooks.org/handle/20.500.12854/32828 95 01 3095 https://directory.doabooks.org/handle/20.500.12854/32828 105 01 0841 https://directory.doabooks.org/handle/20.500.12854/32828 110 01 3110 Open Access https://directory.doabooks.org/handle/20.500.12854/32828 130 01 0700 Open Access https://directory.doabooks.org/handle/20.500.12854/32828 131 01 3131 https://directory.doabooks.org/handle/20.500.12854/32828 136 01 3526 Open Access https://directory.doabooks.org/handle/20.500.12854/32828 161 01 0960 https://directory.doabooks.org/handle/20.500.12854/32828 LF 213 01 0551 https://directory.doabooks.org/handle/20.500.12854/32828 230 01 0552 https://directory.doabooks.org/handle/20.500.12854/32828 283 01 3283 https://directory.doabooks.org/handle/20.500.12854/32828 285 01 0517 Open Access https://directory.doabooks.org/handle/20.500.12854/32828 293 01 3293 https://directory.doabooks.org/handle/20.500.12854/32828 LF 370 01 4370 https://directory.doabooks.org/handle/20.500.12854/32828 635 01 3635 https://directory.doabooks.org/handle/20.500.12854/32828 808 01 4808 Volltextzugang https://directory.doabooks.org/handle/20.500.12854/32828 2011 01 DE-16 https://directory.doabooks.org/handle/20.500.12854/32828 2034 01 DE-Rt2 https://directory.doabooks.org/handle/20.500.12854/32828 2037 01 DE-747 https://directory.doabooks.org/handle/20.500.12854/32828 2050 01 DE-Zi4 https://directory.doabooks.org/handle/20.500.12854/32828 2108 01 DE-991 https://directory.doabooks.org/handle/20.500.12854/32828 20 01 0084 OLR-DOAB 22 01 0018 OLR-ZDB-94-OAB 23 01 0830 olr-doab 24 01 0008 OLR-doab 24 01 0008 olr-frei 30 01 0104 OLR-OAB 60 01 0705 OPENAccess 63 01 3401 E-Books LF GBV-DOAB 72 01 0035 OLR-ZDB-94-OAB 90 01 3090 OLR-HILoapen 91 01 3091 OLR-DOAB 92 01 0033 OLR-Open Access DOAB 95 01 3095 OLR-OAB 105 01 0841 OLR-OAB 110 01 3110 OLR-DOAB 130 01 0700 OLR-DOAB 131 01 3131 OLR-OA-DOAB 136 01 3526 OLR-DOAB 161 01 0960 OLR-DOAB 213 01 0551 OLR-DOAB 230 01 0552 OLR-DOAB 285 01 0517 OLR-DOAB 293 01 3293 OLR-DOAB 370 01 4370 OLR-FREE 370 01 4370 olr-ebook ZDB-94-OAB 635 01 3635 OLR-DOAB 808 01 4808 OLR-DOAB |
| allfieldsGer |
9780429436475 978-0-429-43647-5 20.500.12854/32828 hdl (DE-627)1778511163 (DE-599)KEP069388636 (OCoLC)1193040949 (DOAB)32828 (EBP)069388636 DE-627 ger DE-627 rakwb eng RBK bicssc RGC bicssc RNC bicssc TQ bicssc Hoelzle, Martin verfasserin aut Chapter 8 The Status and Role of the alpine Cryosphere in Central Asia [Erscheinungsort nicht ermittelbar] Taylor & Francis 2019 1 Online-Ressource (23 p.) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Open Access Unrestricted online access star The alpine cryosphere including snow, glaciers and permafrost are critical to water management in the Aral Sea Basin (ASB) and larger Central Asia (CA) under changing climate: as they store large amounts of water in its solid forms. Most cryospheric components in the Aral Sea Basin are close to melting point, and hence very vulnerable to a slight increase in air temperature with significant consequences to long-term water availability and to water resources variability and extremes. Current knowledge about different components of cryosphere and their connection to climate in the Basin and in the entire Central Asia, varies. While it is advanced in the topics of snow and glaciers, knowledge on permafrost it rather limited. Observed trends in runoff point in the direction of increasing water availability in July and August at least until mid-century and increasing possibility for water storage in reservoirs and aquifers. However, eventually this will change as glaciers waste away. Future runoff may change considerably after mid-century and start to decline if not compensated by increasing precipitation. Cryosphere monitoring systems are the basis for sound estimates of water availability and water-related hazards associated with snow, glaciers and permafrost. They require a well-distributed observational network for all cryospheric variables. Such systems need to be re-established in the Basin after the breakup of the Soviet Union in the early 1990s. This process is slowly emerging in the region. Collaboration between local operational hydro-meteorological services and academic sector, and with international research networks may improving the observing capabilities in high mountain regions of CA Asia in general and the ASB specifically Creative Commons by-nc-nd/4.0 cc English Hydrology & the hydrosphere Human geography Applied ecology Environmental science, engineering & technology Barandun, Martina verfasserin aut Bolch, Tobias verfasserin aut Fiddes, Joel verfasserin aut Gafurov, Abror verfasserin aut Muccione, Veruska verfasserin aut Saks, Tomas verfasserin aut Shahgedanova, Maria verfasserin aut Smakhtin, Vladimir herausgeberin edt https://directory.doabooks.org/handle/20.500.12854/32828 X:DOAB Verlag teilw. kostenfrei ZDB-94-OAB GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_24 ISIL_DE-8 GBV_ILN_30 ISIL_DE-104 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_72 ISIL_DE-35 GBV_ILN_90 ISIL_DE-Hil2 GBV_ILN_91 ISIL_DE-HIL3 GBV_ILN_92 ISIL_DE-33 GBV_ILN_95 ISIL_DE-542 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_130 ISIL_DE-700 GBV_ILN_131 ISIL_DE-Va1 GBV_ILN_136 ISIL_DE-Wis1 GBV_ILN_161 ISIL_DE-960 GBV_ILN_213 ISIL_DE-551 GBV_ILN_230 ISIL_DE-552 GBV_ILN_283 ISIL_DE-Ha163 GBV_ILN_285 ISIL_DE-517 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_635 ISIL_DE-B2138 GBV_ILN_808 GBV_ILN_2011 ISIL_DE-16 GBV_ILN_2018 ISIL_DE-31 GBV_ILN_2034 ISIL_DE-Rt2 GBV_ILN_2037 ISIL_DE-747 GBV_ILN_2050 ISIL_DE-Zi4 GBV_ILN_2108 ISIL_DE-991 BO 20 01 0084 4012036963 OLR-DOAB z 01-12-21 22 01 0018 4006127898 OLR-ZDB-94-OAB DOAB Directory of Open Access Books zu 25-11-21 23 01 0830 4006646275 olr-doab f z 25-11-21 24 01 0008 4060128872 OLR-doab z 15-02-22 30 01 0104 4584174075 OLR-OAB Open Access, Directory of Open Access Books (DOAB) z 28-09-24 60 01 0705 4275956613 OPENAccess Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. Nur für Angehörige der HSU: Volltextzugang von außerhalb des Campus mit Anmeldung über Shibboleth mit Ihrer Bibliothekskennung z 24-02-23 63 01 3401 4106581825 E-Books LF GBV-DOAB z 30-03-22 72 01 0035 4104579920 OLR-ZDB-94-OAB DOAB Directory of Open Access Books z 28-03-22 90 01 3090 4106373564 OLR-HILoapen z 29-03-22 91 01 3091 4011353450 OLR-DOAB DOAB Directory of Open Access Books z 01-12-21 92 01 0033 4110730058 OLR-Open Access DOAB Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. Das Ebook ist frei zugänglich. z 02-04-22 95 01 3095 4342224593 OLR-OAB Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. z 23-06-23 105 01 0841 4007106673 OLR-OAB Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. z 25-11-21 110 01 3110 4584412642 OLR-DOAB Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. Open Access z 28-09-24 130 01 0700 4145767950 OLR-DOAB z 08-06-22 131 01 3131 4465754078 OLR-OA-DOAB Bitte beachten Sie die Nutzungsbedingungen und Copyright-Bestimmungen des Verlages/Herausgebers. z 23-01-24 136 01 3526 4005670598 OLR-DOAB z 24-11-21 161 01 0960 4150912017 OLR-DOAB DOAB Directory of Open Access Books z 16-06-22 213 01 0551 4108551095 OLR-DOAB DOAB Directory of Open Access Books z 31-03-22 230 01 0552 4123489311 OLR-DOAB DOAB Directory of Open Access Books z 27-04-22 283 01 3283 4157068017 Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. z 28-06-22 285 01 0517 4050295776 OLR-DOAB z 03-02-22 293 01 3293 4153708879 OLR-DOAB DOAB Directory of Open Access Books z 21-06-22 370 01 4370 412556289X OLR-FREE Kostenloser Zugriff z 28-04-22 635 01 3635 4509870965 OLR-DOAB Open Access. Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. z 10-04-24 808 01 4808 4158104750 OLR-DOAB DOAB Directory of Open Access Books zg 29-06-22 2011 01 DE-16 4025455676 00 --%%-- --%%-- --%%-- --%%-- l01 22-12-21 2018 01 DE-31 4033386645 00 --%%-- --%%-- --%%-- n Der Zugriff ist kostenfrei möglich. l01 11-01-22 2034 01 DE-Rt2 4014392538 00 --%%-- eBook n n frei zugänglich l01 05-12-21 2037 01 DE-747 434562469X 00 --%%-- eBook OAPEN Foundation OpenAccess --%%-- n Im Internet frei verfügbar l01 30-06-23 2050 01 DE-Zi4 4091562442 00 --%%-- --%%-- --%%-- n Elektronischer Volltext - Open Access l01 16-03-22 2108 01 DE-991 4096793248 00 --%%-- eBook DOAB --%%-- n Elektronischer Volltext - Campuslizenz l01 20-03-22 20 01 0084 https://directory.doabooks.org/handle/20.500.12854/32828 22 01 0018 Volltextzugang https://directory.doabooks.org/handle/20.500.12854/32828 23 01 0830 https://directory.doabooks.org/handle/20.500.12854/32828 24 01 0008 https://directory.doabooks.org/handle/20.500.12854/32828 30 01 0104 https://directory.doabooks.org/handle/20.500.12854/32828 60 01 0705 https://directory.doabooks.org/handle/20.500.12854/32828 63 01 3401 E-Book https://directory.doabooks.org/handle/20.500.12854/32828 72 01 0035 https://directory.doabooks.org/handle/20.500.12854/32828 90 01 3090 https://directory.doabooks.org/handle/20.500.12854/32828 91 01 3091 https://directory.doabooks.org/handle/20.500.12854/32828 92 01 0033 https://directory.doabooks.org/handle/20.500.12854/32828 95 01 3095 https://directory.doabooks.org/handle/20.500.12854/32828 105 01 0841 https://directory.doabooks.org/handle/20.500.12854/32828 110 01 3110 Open Access https://directory.doabooks.org/handle/20.500.12854/32828 130 01 0700 Open Access https://directory.doabooks.org/handle/20.500.12854/32828 131 01 3131 https://directory.doabooks.org/handle/20.500.12854/32828 136 01 3526 Open Access https://directory.doabooks.org/handle/20.500.12854/32828 161 01 0960 https://directory.doabooks.org/handle/20.500.12854/32828 LF 213 01 0551 https://directory.doabooks.org/handle/20.500.12854/32828 230 01 0552 https://directory.doabooks.org/handle/20.500.12854/32828 283 01 3283 https://directory.doabooks.org/handle/20.500.12854/32828 285 01 0517 Open Access https://directory.doabooks.org/handle/20.500.12854/32828 293 01 3293 https://directory.doabooks.org/handle/20.500.12854/32828 LF 370 01 4370 https://directory.doabooks.org/handle/20.500.12854/32828 635 01 3635 https://directory.doabooks.org/handle/20.500.12854/32828 808 01 4808 Volltextzugang https://directory.doabooks.org/handle/20.500.12854/32828 2011 01 DE-16 https://directory.doabooks.org/handle/20.500.12854/32828 2034 01 DE-Rt2 https://directory.doabooks.org/handle/20.500.12854/32828 2037 01 DE-747 https://directory.doabooks.org/handle/20.500.12854/32828 2050 01 DE-Zi4 https://directory.doabooks.org/handle/20.500.12854/32828 2108 01 DE-991 https://directory.doabooks.org/handle/20.500.12854/32828 20 01 0084 OLR-DOAB 22 01 0018 OLR-ZDB-94-OAB 23 01 0830 olr-doab 24 01 0008 OLR-doab 24 01 0008 olr-frei 30 01 0104 OLR-OAB 60 01 0705 OPENAccess 63 01 3401 E-Books LF GBV-DOAB 72 01 0035 OLR-ZDB-94-OAB 90 01 3090 OLR-HILoapen 91 01 3091 OLR-DOAB 92 01 0033 OLR-Open Access DOAB 95 01 3095 OLR-OAB 105 01 0841 OLR-OAB 110 01 3110 OLR-DOAB 130 01 0700 OLR-DOAB 131 01 3131 OLR-OA-DOAB 136 01 3526 OLR-DOAB 161 01 0960 OLR-DOAB 213 01 0551 OLR-DOAB 230 01 0552 OLR-DOAB 285 01 0517 OLR-DOAB 293 01 3293 OLR-DOAB 370 01 4370 OLR-FREE 370 01 4370 olr-ebook ZDB-94-OAB 635 01 3635 OLR-DOAB 808 01 4808 OLR-DOAB |
| allfieldsSound |
9780429436475 978-0-429-43647-5 20.500.12854/32828 hdl (DE-627)1778511163 (DE-599)KEP069388636 (OCoLC)1193040949 (DOAB)32828 (EBP)069388636 DE-627 ger DE-627 rakwb eng RBK bicssc RGC bicssc RNC bicssc TQ bicssc Hoelzle, Martin verfasserin aut Chapter 8 The Status and Role of the alpine Cryosphere in Central Asia [Erscheinungsort nicht ermittelbar] Taylor & Francis 2019 1 Online-Ressource (23 p.) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Open Access Unrestricted online access star The alpine cryosphere including snow, glaciers and permafrost are critical to water management in the Aral Sea Basin (ASB) and larger Central Asia (CA) under changing climate: as they store large amounts of water in its solid forms. Most cryospheric components in the Aral Sea Basin are close to melting point, and hence very vulnerable to a slight increase in air temperature with significant consequences to long-term water availability and to water resources variability and extremes. Current knowledge about different components of cryosphere and their connection to climate in the Basin and in the entire Central Asia, varies. While it is advanced in the topics of snow and glaciers, knowledge on permafrost it rather limited. Observed trends in runoff point in the direction of increasing water availability in July and August at least until mid-century and increasing possibility for water storage in reservoirs and aquifers. However, eventually this will change as glaciers waste away. Future runoff may change considerably after mid-century and start to decline if not compensated by increasing precipitation. Cryosphere monitoring systems are the basis for sound estimates of water availability and water-related hazards associated with snow, glaciers and permafrost. They require a well-distributed observational network for all cryospheric variables. Such systems need to be re-established in the Basin after the breakup of the Soviet Union in the early 1990s. This process is slowly emerging in the region. Collaboration between local operational hydro-meteorological services and academic sector, and with international research networks may improving the observing capabilities in high mountain regions of CA Asia in general and the ASB specifically Creative Commons by-nc-nd/4.0 cc English Hydrology & the hydrosphere Human geography Applied ecology Environmental science, engineering & technology Barandun, Martina verfasserin aut Bolch, Tobias verfasserin aut Fiddes, Joel verfasserin aut Gafurov, Abror verfasserin aut Muccione, Veruska verfasserin aut Saks, Tomas verfasserin aut Shahgedanova, Maria verfasserin aut Smakhtin, Vladimir herausgeberin edt https://directory.doabooks.org/handle/20.500.12854/32828 X:DOAB Verlag teilw. kostenfrei ZDB-94-OAB GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_24 ISIL_DE-8 GBV_ILN_30 ISIL_DE-104 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_72 ISIL_DE-35 GBV_ILN_90 ISIL_DE-Hil2 GBV_ILN_91 ISIL_DE-HIL3 GBV_ILN_92 ISIL_DE-33 GBV_ILN_95 ISIL_DE-542 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_130 ISIL_DE-700 GBV_ILN_131 ISIL_DE-Va1 GBV_ILN_136 ISIL_DE-Wis1 GBV_ILN_161 ISIL_DE-960 GBV_ILN_213 ISIL_DE-551 GBV_ILN_230 ISIL_DE-552 GBV_ILN_283 ISIL_DE-Ha163 GBV_ILN_285 ISIL_DE-517 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_635 ISIL_DE-B2138 GBV_ILN_808 GBV_ILN_2011 ISIL_DE-16 GBV_ILN_2018 ISIL_DE-31 GBV_ILN_2034 ISIL_DE-Rt2 GBV_ILN_2037 ISIL_DE-747 GBV_ILN_2050 ISIL_DE-Zi4 GBV_ILN_2108 ISIL_DE-991 BO 20 01 0084 4012036963 OLR-DOAB z 01-12-21 22 01 0018 4006127898 OLR-ZDB-94-OAB DOAB Directory of Open Access Books zu 25-11-21 23 01 0830 4006646275 olr-doab f z 25-11-21 24 01 0008 4060128872 OLR-doab z 15-02-22 30 01 0104 4584174075 OLR-OAB Open Access, Directory of Open Access Books (DOAB) z 28-09-24 60 01 0705 4275956613 OPENAccess Vervielfältigungen (z.B. 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code="a">GBV_ILN_293</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-960-3</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_370</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-1373</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_635</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-B2138</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_808</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2011</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-16</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2018</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-31</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2034</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-Rt2</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2037</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-747</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2050</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-Zi4</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2108</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-991</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">BO</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">20</subfield><subfield code="1">01</subfield><subfield code="x">0084</subfield><subfield code="b">4012036963</subfield><subfield code="h">OLR-DOAB</subfield><subfield code="y">z</subfield><subfield code="z">01-12-21</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">22</subfield><subfield code="1">01</subfield><subfield code="x">0018</subfield><subfield code="b">4006127898</subfield><subfield code="h">OLR-ZDB-94-OAB</subfield><subfield code="k">DOAB Directory of Open Access Books</subfield><subfield code="y">zu</subfield><subfield code="z">25-11-21</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">23</subfield><subfield code="1">01</subfield><subfield code="x">0830</subfield><subfield code="b">4006646275</subfield><subfield code="h">olr-doab</subfield><subfield code="u">f</subfield><subfield code="y">z</subfield><subfield code="z">25-11-21</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">24</subfield><subfield code="1">01</subfield><subfield code="x">0008</subfield><subfield code="b">4060128872</subfield><subfield code="h">OLR-doab</subfield><subfield code="y">z</subfield><subfield code="z">15-02-22</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">30</subfield><subfield code="1">01</subfield><subfield code="x">0104</subfield><subfield code="b">4584174075</subfield><subfield code="h">OLR-OAB</subfield><subfield code="k">Open Access, Directory of Open Access Books (DOAB)</subfield><subfield code="y">z</subfield><subfield code="z">28-09-24</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">60</subfield><subfield code="1">01</subfield><subfield code="x">0705</subfield><subfield code="b">4275956613</subfield><subfield code="h">OPENAccess</subfield><subfield code="k">Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots.</subfield><subfield code="k">Nur für Angehörige der HSU: Volltextzugang von außerhalb des Campus mit Anmeldung über Shibboleth mit Ihrer Bibliothekskennung</subfield><subfield code="y">z</subfield><subfield code="z">24-02-23</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">63</subfield><subfield code="1">01</subfield><subfield code="x">3401</subfield><subfield code="b">4106581825</subfield><subfield code="h">E-Books LF GBV-DOAB</subfield><subfield code="y">z</subfield><subfield code="z">30-03-22</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">72</subfield><subfield code="1">01</subfield><subfield code="x">0035</subfield><subfield code="b">4104579920</subfield><subfield code="h">OLR-ZDB-94-OAB</subfield><subfield code="k">DOAB Directory of Open Access Books</subfield><subfield code="y">z</subfield><subfield code="z">28-03-22</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">90</subfield><subfield code="1">01</subfield><subfield code="x">3090</subfield><subfield code="b">4106373564</subfield><subfield code="h">OLR-HILoapen</subfield><subfield code="y">z</subfield><subfield code="z">29-03-22</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">91</subfield><subfield code="1">01</subfield><subfield code="x">3091</subfield><subfield code="b">4011353450</subfield><subfield code="h">OLR-DOAB</subfield><subfield code="k">DOAB Directory of Open Access Books</subfield><subfield code="y">z</subfield><subfield code="z">01-12-21</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">92</subfield><subfield code="1">01</subfield><subfield code="x">0033</subfield><subfield code="b">4110730058</subfield><subfield code="h">OLR-Open Access DOAB</subfield><subfield code="k">Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. Das Ebook ist frei zugänglich.</subfield><subfield code="y">z</subfield><subfield code="z">02-04-22</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">95</subfield><subfield code="1">01</subfield><subfield code="x">3095</subfield><subfield code="b">4342224593</subfield><subfield code="h">OLR-OAB</subfield><subfield code="k">Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt.</subfield><subfield code="y">z</subfield><subfield code="z">23-06-23</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">105</subfield><subfield code="1">01</subfield><subfield code="x">0841</subfield><subfield code="b">4007106673</subfield><subfield code="h">OLR-OAB</subfield><subfield code="k">Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt.</subfield><subfield code="y">z</subfield><subfield code="z">25-11-21</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">110</subfield><subfield code="1">01</subfield><subfield code="x">3110</subfield><subfield code="b">4584412642</subfield><subfield code="h">OLR-DOAB</subfield><subfield code="k">Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt.</subfield><subfield code="k">Open Access</subfield><subfield code="y">z</subfield><subfield code="z">28-09-24</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">130</subfield><subfield code="1">01</subfield><subfield code="x">0700</subfield><subfield code="b">4145767950</subfield><subfield code="h">OLR-DOAB</subfield><subfield code="y">z</subfield><subfield code="z">08-06-22</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">131</subfield><subfield code="1">01</subfield><subfield code="x">3131</subfield><subfield code="b">4465754078</subfield><subfield code="h">OLR-OA-DOAB</subfield><subfield code="k">Bitte beachten Sie die Nutzungsbedingungen und Copyright-Bestimmungen des Verlages/Herausgebers.</subfield><subfield code="y">z</subfield><subfield code="z">23-01-24</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">136</subfield><subfield code="1">01</subfield><subfield code="x">3526</subfield><subfield code="b">4005670598</subfield><subfield code="h">OLR-DOAB</subfield><subfield code="y">z</subfield><subfield code="z">24-11-21</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">161</subfield><subfield code="1">01</subfield><subfield code="x">0960</subfield><subfield code="b">4150912017</subfield><subfield code="h">OLR-DOAB</subfield><subfield code="k">DOAB Directory of Open Access Books</subfield><subfield code="y">z</subfield><subfield code="z">16-06-22</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">213</subfield><subfield code="1">01</subfield><subfield code="x">0551</subfield><subfield code="b">4108551095</subfield><subfield code="h">OLR-DOAB</subfield><subfield code="k">DOAB Directory of Open Access Books</subfield><subfield code="y">z</subfield><subfield code="z">31-03-22</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">230</subfield><subfield code="1">01</subfield><subfield code="x">0552</subfield><subfield code="b">4123489311</subfield><subfield code="h">OLR-DOAB</subfield><subfield code="k">DOAB Directory of Open Access Books</subfield><subfield code="y">z</subfield><subfield code="z">27-04-22</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">283</subfield><subfield code="1">01</subfield><subfield code="x">3283</subfield><subfield code="b">4157068017</subfield><subfield code="k">Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt.</subfield><subfield code="y">z</subfield><subfield code="z">28-06-22</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">285</subfield><subfield code="1">01</subfield><subfield code="x">0517</subfield><subfield code="b">4050295776</subfield><subfield code="h">OLR-DOAB</subfield><subfield code="y">z</subfield><subfield code="z">03-02-22</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">293</subfield><subfield code="1">01</subfield><subfield code="x">3293</subfield><subfield code="b">4153708879</subfield><subfield code="h">OLR-DOAB</subfield><subfield code="k">DOAB Directory of Open Access Books</subfield><subfield code="y">z</subfield><subfield code="z">21-06-22</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">370</subfield><subfield code="1">01</subfield><subfield code="x">4370</subfield><subfield code="b">412556289X</subfield><subfield code="h">OLR-FREE</subfield><subfield code="k">Kostenloser Zugriff</subfield><subfield code="y">z</subfield><subfield code="z">28-04-22</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">635</subfield><subfield code="1">01</subfield><subfield code="x">3635</subfield><subfield code="b">4509870965</subfield><subfield code="h">OLR-DOAB</subfield><subfield code="k">Open Access. Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt.</subfield><subfield code="y">z</subfield><subfield code="z">10-04-24</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">808</subfield><subfield code="1">01</subfield><subfield code="x">4808</subfield><subfield code="b">4158104750</subfield><subfield code="h">OLR-DOAB</subfield><subfield code="k">DOAB Directory of Open Access Books</subfield><subfield code="y">zg</subfield><subfield code="z">29-06-22</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">2011</subfield><subfield code="1">01</subfield><subfield code="x">DE-16</subfield><subfield code="b">4025455676</subfield><subfield code="c">00</subfield><subfield code="f">--%%--</subfield><subfield code="d">--%%--</subfield><subfield code="e">--%%--</subfield><subfield code="j">--%%--</subfield><subfield code="y">l01</subfield><subfield code="z">22-12-21</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">2018</subfield><subfield code="1">01</subfield><subfield code="x">DE-31</subfield><subfield code="b">4033386645</subfield><subfield code="c">00</subfield><subfield code="f">--%%--</subfield><subfield code="d">--%%--</subfield><subfield code="e">--%%--</subfield><subfield code="j">n</subfield><subfield code="k">Der Zugriff ist kostenfrei möglich.</subfield><subfield code="y">l01</subfield><subfield code="z">11-01-22</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">2034</subfield><subfield code="1">01</subfield><subfield code="x">DE-Rt2</subfield><subfield code="b">4014392538</subfield><subfield code="c">00</subfield><subfield code="f">--%%--</subfield><subfield code="d">eBook</subfield><subfield code="e">n</subfield><subfield code="j">n</subfield><subfield code="k">frei zugänglich</subfield><subfield code="y">l01</subfield><subfield code="z">05-12-21</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">2037</subfield><subfield code="1">01</subfield><subfield code="x">DE-747</subfield><subfield code="b">434562469X</subfield><subfield code="c">00</subfield><subfield code="f">--%%--</subfield><subfield code="d">eBook OAPEN Foundation OpenAccess</subfield><subfield code="e">--%%--</subfield><subfield code="j">n</subfield><subfield code="k">Im Internet frei verfügbar</subfield><subfield code="y">l01</subfield><subfield code="z">30-06-23</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">2050</subfield><subfield code="1">01</subfield><subfield code="x">DE-Zi4</subfield><subfield code="b">4091562442</subfield><subfield code="c">00</subfield><subfield code="f">--%%--</subfield><subfield code="d">--%%--</subfield><subfield code="e">--%%--</subfield><subfield code="j">n</subfield><subfield code="k">Elektronischer Volltext - Open Access</subfield><subfield code="y">l01</subfield><subfield code="z">16-03-22</subfield></datafield><datafield tag="980" ind1=" " 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Chapter 8 The Status and Role of the alpine Cryosphere in Central Asia |
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The alpine cryosphere including snow, glaciers and permafrost are critical to water management in the Aral Sea Basin (ASB) and larger Central Asia (CA) under changing climate: as they store large amounts of water in its solid forms. Most cryospheric components in the Aral Sea Basin are close to melting point, and hence very vulnerable to a slight increase in air temperature with significant consequences to long-term water availability and to water resources variability and extremes. Current knowledge about different components of cryosphere and their connection to climate in the Basin and in the entire Central Asia, varies. While it is advanced in the topics of snow and glaciers, knowledge on permafrost it rather limited. Observed trends in runoff point in the direction of increasing water availability in July and August at least until mid-century and increasing possibility for water storage in reservoirs and aquifers. However, eventually this will change as glaciers waste away. Future runoff may change considerably after mid-century and start to decline if not compensated by increasing precipitation. Cryosphere monitoring systems are the basis for sound estimates of water availability and water-related hazards associated with snow, glaciers and permafrost. They require a well-distributed observational network for all cryospheric variables. Such systems need to be re-established in the Basin after the breakup of the Soviet Union in the early 1990s. This process is slowly emerging in the region. Collaboration between local operational hydro-meteorological services and academic sector, and with international research networks may improving the observing capabilities in high mountain regions of CA Asia in general and the ASB specifically |
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The alpine cryosphere including snow, glaciers and permafrost are critical to water management in the Aral Sea Basin (ASB) and larger Central Asia (CA) under changing climate: as they store large amounts of water in its solid forms. Most cryospheric components in the Aral Sea Basin are close to melting point, and hence very vulnerable to a slight increase in air temperature with significant consequences to long-term water availability and to water resources variability and extremes. Current knowledge about different components of cryosphere and their connection to climate in the Basin and in the entire Central Asia, varies. While it is advanced in the topics of snow and glaciers, knowledge on permafrost it rather limited. Observed trends in runoff point in the direction of increasing water availability in July and August at least until mid-century and increasing possibility for water storage in reservoirs and aquifers. However, eventually this will change as glaciers waste away. Future runoff may change considerably after mid-century and start to decline if not compensated by increasing precipitation. Cryosphere monitoring systems are the basis for sound estimates of water availability and water-related hazards associated with snow, glaciers and permafrost. They require a well-distributed observational network for all cryospheric variables. Such systems need to be re-established in the Basin after the breakup of the Soviet Union in the early 1990s. This process is slowly emerging in the region. Collaboration between local operational hydro-meteorological services and academic sector, and with international research networks may improving the observing capabilities in high mountain regions of CA Asia in general and the ASB specifically |
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The alpine cryosphere including snow, glaciers and permafrost are critical to water management in the Aral Sea Basin (ASB) and larger Central Asia (CA) under changing climate: as they store large amounts of water in its solid forms. Most cryospheric components in the Aral Sea Basin are close to melting point, and hence very vulnerable to a slight increase in air temperature with significant consequences to long-term water availability and to water resources variability and extremes. Current knowledge about different components of cryosphere and their connection to climate in the Basin and in the entire Central Asia, varies. While it is advanced in the topics of snow and glaciers, knowledge on permafrost it rather limited. Observed trends in runoff point in the direction of increasing water availability in July and August at least until mid-century and increasing possibility for water storage in reservoirs and aquifers. However, eventually this will change as glaciers waste away. Future runoff may change considerably after mid-century and start to decline if not compensated by increasing precipitation. Cryosphere monitoring systems are the basis for sound estimates of water availability and water-related hazards associated with snow, glaciers and permafrost. They require a well-distributed observational network for all cryospheric variables. Such systems need to be re-established in the Basin after the breakup of the Soviet Union in the early 1990s. This process is slowly emerging in the region. Collaboration between local operational hydro-meteorological services and academic sector, and with international research networks may improving the observing capabilities in high mountain regions of CA Asia in general and the ASB specifically |
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Most cryospheric components in the Aral Sea Basin are close to melting point, and hence very vulnerable to a slight increase in air temperature with significant consequences to long-term water availability and to water resources variability and extremes. Current knowledge about different components of cryosphere and their connection to climate in the Basin and in the entire Central Asia, varies. While it is advanced in the topics of snow and glaciers, knowledge on permafrost it rather limited. Observed trends in runoff point in the direction of increasing water availability in July and August at least until mid-century and increasing possibility for water storage in reservoirs and aquifers. However, eventually this will change as glaciers waste away. Future runoff may change considerably after mid-century and start to decline if not compensated by increasing precipitation. Cryosphere monitoring systems are the basis for sound estimates of water availability and water-related hazards associated with snow, glaciers and permafrost. They require a well-distributed observational network for all cryospheric variables. Such systems need to be re-established in the Basin after the breakup of the Soviet Union in the early 1990s. This process is slowly emerging in the region. 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