Historical and future antarctic precipitation based on CMIP5 models, reanalysis data and in situ measurements /
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| Main Author: | |
|---|---|
| Format: | Thesis Book |
| Language: | English |
| Published: |
2020.
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| Subjects: | |
| Online Access: | http://studentsrepo.um.edu.my/12096/ |
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| 001 | u1140108 | ||
| 003 | SIRSI | ||
| 005 | 202012171557 | ||
| 008 | 201217s2020 my a m 000 0 eng | ||
| 040 | |a UMM |d AUM |e rda | ||
| 043 | |a t------ | ||
| 090 | |a Q180 |b UMP 2020 Tan | ||
| 100 | 1 | |a Tang, Malcolm Song Yii, |e author. | |
| 245 | 1 | 0 | |a Historical and future antarctic precipitation based on CMIP5 models, reanalysis data and in situ measurements / |c Malcolm Tang Siong Yii. |
| 264 | 1 | |c 2020. | |
| 300 | |a xxiv, 183 leaves : |b illustrations ; |c 30 cm | ||
| 336 | |a text |2 rdacontent | ||
| 336 | |a still image |2 rdacontent | ||
| 337 | |a unmediated |2 rdamedia | ||
| 337 | |a computer |2 rdamedia | ||
| 338 | |a volume |2 rdacarrier | ||
| 338 | |a computer disc |2 rdacarrier | ||
| 502 | |b Ph.D. |c Institut Pengajian Termaju, Universiti Malaya |d 2020. | ||
| 504 | |a Bibliography: leaves 158-171. | ||
| 530 | |a Also issued in CD. | ||
| 650 | 0 | |a Precipitation (Meteorology) |z Antarctica |x Measurement. | |
| 650 | 0 | |a Precipitation forecasting |z Antarctica. | |
| 650 | 0 | |a Sea ice |z Antarctica. | |
| 650 | 0 | |a Climatic changes |x Computer simulation. | |
| 650 | 0 | |a Ocean-atmosphere interaction |z Antarctica. | |
| 651 | 0 | |a Antarctica |x Environmental conditions. | |
| 710 | 2 | |a Universiti Malaya. |b Institut Pengajian Termaju, |e degree granting institution. | |
| 856 | 4 | 1 | |u http://studentsrepo.um.edu.my/12096/ |
| 900 | |a NNANS NSM | ||
| 596 | |a 1 25 | ||
| 999 | |a Q180 UMP 2020 TAN |w LC |c 1 |i A517669760 |f 28/12/2020 |g 1 |l STACKS |m P01UTAMA |r Y |s Y |t TESIS |u 28/12/2020 |1 STEM | ||
| 999 | |a Q180 UMP 2020 TAN |w LC |c 1 |i A517669795 |f 27/1/2021 |g 1 |l STACKS |m P25UMARCHI |r N |s Y |t CD |u 27/1/2021 |1 AHSS |o .STAFF. MST-CD5003 | ||
