| ²é¿´: 905 | »Ø¸´: 3 | ||
| µ±Ç°Ö»ÏÔʾÂú×ãÖ¸¶¨Ìõ¼þµÄ»ØÌû£¬µã»÷ÕâÀï²é¿´±¾»°ÌâµÄËùÓлØÌû | ||
ltzahÒø³æ (³õÈëÎÄ̳)
|
[ÇóÖú]
ÈçºÎÆÀ¹ÀµØÐÎÒòËØ¶ÔÓÚkriging²åÖµ½á¹ûµÄ²»È·¶¨ÐÔ ÒÑÓÐ1È˲ÎÓë
|
|
|
¸÷λ´óÏÀ£¬ÎÒһƪÎÄÕÂÓöà¸öÆøÏóÕ¾µãÊý¾Ý½øÐÐkriging²åÖµ£¬µÃµ½µÄ½á¹û£¬Éó¸åÈ˽¨ÒéͬʱÆÀ¹ÀµØÐεÈÒòËØ¶ÔÓÚ²åÖµ½á¹û²»È·¶¨ÐÔµÄÓ°Ï죬ÎÒ¾ßÌå¸Ãʲô×öÄØ£¿Éó¸åÈ˵ľßÌåÒâ¼ûÈçÏ£º From the study area size and the number of weather stations one can estimate that the average linear distance between neighbouring stations is of order 80 km. For pixels interpolated by Kriging, there can potentially be a lot of uncertainty in the meteorological variables due to regional heterogeneity (topography, evaporation from large water bodies, etc.) Is it possible to assess the uncertainty of the meteorological variables due to these effects? |
» ²ÂÄãϲ»¶
¶¨Á˶¨ÁË£¬Ã÷Ìì³ö½á¹û£¡2025 ¹ú×ÔÈ»»ù½ð½á¹û¼´½«½ÒÏþ£¬²éѯ¹¥ÂÔ¿´ÕâÀï
ÒѾÓÐ107È˻ظ´
2025¹ú¼Ò×ÔÈ»¿ÆÑ§»ù½ð·Å°ñʱ¼ä£¬¸ù¾Ý¹Ù·½»ØÓ¦£¬8ÔÂ15ÈÕ»ù±¾Ã»Ï·ÁË
ÒѾÓÐ5È˻ظ´
µØÖÊѧÂÛÎÄÈóÉ«/·ÒëÔõôÊÕ·Ñ?
ÒѾÓÐ107È˻ظ´
¸÷λδÀ´ÔºÊ¿°ïæ¿´¿´ÆÀÉóÒâ¼û
ÒѾÓÐ9È˻ظ´
¡¶·ç´µ¹ýÈÕ³£µÄ·ì϶¡·
ÒѾÓÐ0È˻ظ´
Î÷ÄϿƼ¼´óѧ µ÷¼Á ÃàÑô
ÒѾÓÐ10È˻ظ´
É¢½ð±Ò£¬Çó»ù½ðÖб꣡£¡
ÒѾÓÐ40È˻ظ´
poseur
Ìú³æ (СÓÐÃûÆø)
- Ó¦Öú: 1 (Ó×¶ùÔ°)
- ½ð±Ò: 112.5
- Ìû×Ó: 104
- ÔÚÏß: 42.1Сʱ
- ³æºÅ: 344917
- ×¢²á: 2007-04-14
- רҵ: µØÀíÐÅϢϵͳ
3Â¥2017-02-08 18:35:29
zyccau
гæ (СÓÐÃûÆø)
- Ó¦Öú: 1 (Ó×¶ùÔ°)
- ½ð±Ò: 4.6
- Ìû×Ó: 62
- ÔÚÏß: 75.4Сʱ
- ³æºÅ: 2307134
- ×¢²á: 2013-02-28
- רҵ: ×ÔÈ»µØÀíѧ
|
¸öÈË×î½üÒ²±»¸ÃÎÊÌâÀ§ÈÅ£¬Èç¹û½øÐвåÖµ¼ÆË㣬ÎÞ·¨±ÜÃâµØÐÎÒòËØµÄÓ°Ïì ·¢×ÔСľ³æAndroid¿Í»§¶Ë |
2Â¥2016-06-15 10:28:46
scapeÄê
гæ (СÓÐÃûÆø)
- Ó¦Öú: 0 (Ó×¶ùÔ°)
- ½ð±Ò: 73.3
- É¢½ð: 68
- ºì»¨: 1
- Ìû×Ó: 75
- ÔÚÏß: 6.2Сʱ
- ³æºÅ: 8379017
- ×¢²á: 2018-03-26
- ÐÔ±ð: MM
- רҵ: ¾°¹ÛµØÀíѧ
4Â¥2021-05-15 08:58:31













»Ø¸´´ËÂ¥