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Name | CEOP CAMP Himalayas Reference Site |
Metadata Identifier | CEOP_CAMP_Himalayas20230727060140-DIAS20221121113753-en |
Name | Gianni Tartari |
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Organization | CNR-IRSA / Ev-K2-CNR Committee |
Address | Via San Bernardino, 145 , Bergamo, 24126 , Italy |
TEL | +39/035/3230513 |
FAX | +39/035/3230551 |
tartari@irsa.cnr.it |
Name | Elisa Vuillermoz |
---|---|
Organization | Ev-K2-CNR Committee |
Address | Via San Bernardino, 145 , Bergamo, 24126 , Italy |
TEL | +39/035/3230513 |
FAX | +39/035/3230551 |
vuillemoz@evk2cnr.org |
Name | DIAS Office |
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Organization | Japan Agency for Marine-Earth Science and Technology |
Address | 3173-25, Showa-Cho, Kanazawa-ku, Yokohama-shi, Kanagawa, 236-0001, Japan |
dias-office@diasjp.net |
Name | Gianni Tartari |
---|---|
Organization | CNR-IRSA / Ev-K2-CNR Committee |
tartari@irsa.cnr.it |
Name | Elisa Vuillermoz |
---|---|
Organization | Ev-K2-CNR Committee |
vuillemoz@evk2cnr.org |
Name | Gianni Tartari |
---|---|
Organization | CNR-IRSA / Ev-K2-CNR Committee |
tartari@irsa.cnr.it |
Name | Elisa Vuillermoz |
---|---|
Organization | Ev-K2-CNR Committee |
vuillemoz@evk2cnr.org |
creation : 2010-05-06
revision : 2011-11-22
Intensive meteorological observations in the Khumbu Valley, Nepal Himalayas, have
been conducted since the middle 90's (Ueno et al., 1996; Tartari et al., 1999;
Bertolani et al., 2000; Ueno et al., 2001; Bollasina et al., 2002; Ueno and Pokhrel,
2002) in order to provide long-term monitoring of the monsoon at high altitude. This
area, being located on the windward side of the Range with respect to the Indian
monsoon, is well exposed to the summer winds. The studies conducted have demonstrated
that the region is a significant point of observation both of local climate and large-
scale circulation. A network of Automated Weather Stations (AWSs) has been established
in the Eastern Himalayas: the AWSs are located at different altitudes, over a 40 km
stretch oriented approximately south to north.
climatologyMeteorologyAtmosphere
Begin Date | 2002-10-01 00:00:00 |
End Date | 2009-12-31 23:59:59 |
Temporal Characteristics | Hourly |
North bound latitude | 27.700000 |
West bound longitude | 86.720000 |
Eastbound longitude | 86.820000 |
South bound latitude | 27.960000 |
Keyword Type | Keyword | Keyword thesaurus Name |
---|---|---|
theme | Climate, Water | GEOSS |
Keyword Type | Keyword | Keyword thesaurus Name |
---|---|---|
theme | DIAS > Data Integration and Analysis System | No_Dictionary |
: http://www.eol.ucar.edu/projects/ceop/dm/insitu/sites/ceop_ap/Himalayas/Pyramid/
: http://www.eol.ucar.edu/projects/ceop/dm/insitu/sites/ceop_ap/Himalayas/Lukla/
: http://www.eol.ucar.edu/projects/ceop/dm/insitu/sites/ceop_ap/Himalayas/Namche/
: http://www.eol.ucar.edu/projects/ceop/dm/insitu/sites/ceop_ap/Himalayas/Pheriche/
: http://www.eol.ucar.edu/projects/ceop/dm/insitu/sites/ceop_ap/Himalayas/Syangboche/
file download : https://data.diasjp.net/dl/storages/filelist/dataset:113
name | version | specification |
---|---|---|
PRN | no information | CEOP Unified Format |
Temperature, relative humidity and solar radiation are instantaneous values.
Precipitation is accumulated on the previous hour. Atmospheric pressure is averaged
over the previous hour. Wind speed and direction are the resulting average speed and
direction over the previous hour (calculated by the datalogger by means of data
recorded every 5 seconds): this to minimize data unreliability due to sudden gusts.
Both of them are calculated weighting the frequency distribution of both variables
within each hour.
1. No financial implications are involved for the CEOP reference site data exchange.
2. Commercial use and exploitation of CEOP reference site data is prohibited.
3. Any re-export or transfer of the original data received from the CDA archive to a third party is prohibited.
4. The origin of CEOP reference site data being used for publication of scientific results must be acknowledged and referenced in the publication.
5. CEOP reference site data users are strongly encouraged to establish direct contact with data providers for complete interpretation and analysis of data for publication purposes.
6. Co-authorship of data users and CEOP reference site Principle Investigators on papers making extensive use of CEOP data is justifiable and highly recommended.
see http://www.eol.ucar.edu/projects/ceop/dm/documents/ceop_policy.html
If data provider does not have data policy, DIAS Terms of Service (https://diasjp.net/en/terms/) and DIAS Privacy Policy (https://diasjp.net/en/privacy/) apply.
If there is a conflict between DIAS Terms of Service and data provider's policy, the data provider's policy shall prevail.
A minimum requirement is to reference CEOP as:
The in-situ data is provided under the framework of the "Coordinated Energy and Water Cycle Observations Project (CEOP)."
for the Coordinated Energy and Water Cycle Observations Project data (2005), and as:
The satellite data is provided under the framework of the "Coordinated Enhanced Observing Period (CEOP)."
for the Coordinated Enhanced Observing Period data (2001 - 2004).
If you plan to use this dataset for a conference presentation, paper, journal article, or report etc., please include acknowledgments referred to following examples. If the data provider describes examples of acknowledgments, include them as well.
" In this study, [Name of Dataset] provided by [Name of Data Provider] was utilized. This dataset was also collected and provided under the Data Integration and Analysis System (DIAS), which was developed and operated by a project supported by the Ministry of Education, Culture, Sports, Science and Technology. "
Original data was collected and is provided within the framework of the Ev-K2-CNR/RONAST Joint Scientific and Technological Research Project, funded by Italian Ministries and National Research Council through the Ev-K2-CNR Committee.
Ueno K., and A. P. Pokhrel, 2002: Intra-seasonal air temperature variation in the Nepal
Himalayas, Mausam, 53, 281-288.
Bollasina, M., L. Bertolani, and G. Tartari, 2002: Meteorological observations in the
Khumbu Valley, Nepal Himalayas, 1994-1999, Bull. Glac. Res., 19, 1-11.
Ueno K., R. B. Kayastha, M. R. Chitrakar, O. R. Bajracharya, A. P. Pokhrel, H. Fujinami,
T. Kadota, H. Iida, D. P. Manandhar, M. Hattori, T. Yasunari, and M. Nakawo, 2001:
Meteorological observations during 1994-2000 at the Automatic Weather Station (GEN-AWS)
in Khumbu region, Nepal Himalayas, Bull. Glac. Res., 18, 23-30.
Bertolani, L., M. Bollasina, and G. Tartari, 2000: Recent biennial variability of
meteorological features in the Eastern Highland Himalayas, Geophys. Res. Lett., 17,
2185-2188.
Tartari, G., G. P. Verza, and L. Bertolani, 1999: Meteorological data at the Pyramid
Laboratory. In: A. Lami, R. Mosello, G. Giussani (Eds), Limnology of high altitude
in the Khumbu Valley, Nepal. Documenta Ist. Ital. Idrobiol.
Ueno K., H. Iida, H. Yabuki, K. Seko, A. Sakai, G. S. Lhakupa, R. B. Kayastha, A. P.
Pokhrel, M. L. Shrestha, T. Yasunari, and M. Nakawo, 1996: Establishment of the GEN
Automatic Weather Station (AWS) in Khumbu region, Nepal Himalayas, Bull. Glac. Res.,
14, 13-22.