| ²é¿´: 498 | »Ø¸´: 4 | |||
| µ±Ç°Ö÷ÌâÒѾ´æµµ¡£ | |||
hbqoucľ³æ (ÖªÃû×÷¼Ò)
|
[½»Á÷]
¡¾ÇóÖú¡¿AGU ÎÄÏ×һƪ
|
||
|
Global coastal segmentation and its river catchment contributors: A new look at land-ocean linkage Global coastal segmentation and its river catchment contributors: A new look at land-ocean linkage Michel Meybeck UMR Sisyphe, Universit¨¦ Pierre et Marie Curie, Paris, France Hans H. D¨¹rr UMR Sisyphe, Universit¨¦ Pierre et Marie Curie, Paris, France Charles J. Vörösmarty Water Systems Analysis Group, Complex Systems, University of New Hampshire, Durham, New Hampshire, USA Here we present the COSCATs global database of 151 catchments in exorheic areas. The catchments connect to oceans through coastal segments according to three sets of criteria: natural limits (continents, oceans, regional seas, major capes, and bays), continental shelf topography (sills, basins, island chains), and geophysical dynamics (climate, ocean currents and tectonics). The COSCATs segmentation scheme is designed to improve Earth System analysis and to harmonize reporting of global riverine transfers from land to oceans. Each COSCAT is characterized by its coastal segment limits and length (median 2 400 km), by its catchment characteristics, including area (median 0.45 M km2), width, latitudinal range, runoff average value and direction, including its related physiographic units (n = 500). We apply the COSCAT segmentation to all 151 basins to estimate water discharge and total nitrogen impacts to oceans and find that the average runoff (mm/yr) and N yields (YN in kg km−2 yr−1) range over more than 3 orders of magnitude at this coarse resolution, and that their average population density ranges over 2 orders of magnitude. Hyperactive regions, defined as segments with 5 to 10 times the world average yield (river transfers per unit area of land), are differentially placed for water runoff and total contemporary nitrogen. COSCATs have been designed to facilitate the budget reporting and the analysis of global scale heterogeneity for riverine fluxes and can be applied to other material, such as suspended solids, carbon species or other nutrients, particularly for areas draining into regional seas. Received 21 April 2005; accepted 10 November 2005; published 25 February 2006. Citation: Meybeck, M., H. H. D¨¹rr, and C. J. Vörösmarty (2006), Global coastal segmentation and its river catchment contributors: A new look at land-ocean linkage, Global Biogeochem. Cycles, 20, GB1S90, doi:10.1029/2005GB002540. ºÇºÇ ÓÖÒªÂé·³¸÷λ³æÓÑÁË Ð»Ð» ·Ç³£¸Ðл ÎÒµÄÓÊÏ䣺bangqihu@gmail.com |
» ²ÂÄãϲ»¶
326µ÷¼ÁÌû
ÒѾÓÐ1È˻ظ´
³ÇÏç¹æ»®Ñ§ÕÐÊÕµ÷¼Á 1Ãû
ÒѾÓÐ1È˻ظ´
µØÇòÎïÀíѧºÍ¿Õ¼äÎïÀíѧÂÛÎÄÈóÉ«/·ÒëÔõôÊÕ·Ñ?
ÒѾÓÐ79È˻ظ´
ÇàC×îºóÒ»Ä꣬ɢ½ðÆí¸£°É
ÒѾÓÐ48È˻ظ´
ÎÞ·¨´ÓÕâ·ÝÔ´ÂëÅжÏÏîÄ¿ÊÇ·ñ¡°»ñ×ÊÖúÅú×¼¡±
ÒѾÓÐ11È˻ظ´
ûÖУ¬ÓеãÄÑÊÜ£¬¿ÆÑÐÒ²Ðí¾Íµ½ÕâÁË£¬»Ø¹éÉú»î°É
ÒѾÓÐ15È˻ظ´
¡¾ÕÐÆ¸¡¿¿ÆÑÐÖúÀí+ÎåÏÕÒ»½ð
ÒѾÓÐ20È˻ظ´
ÕÐÆ¸²©Ê¿Ñо¿Éú
ÒѾÓÐ45È˻ظ´

lxj35288
ľ³æ (ÕýʽдÊÖ)
- Ó¦Öú: 0 (Ó×¶ùÔ°)
- ½ð±Ò: 2647.6
- Ìû×Ó: 383
- ÔÚÏß: 13.9Сʱ
- ³æºÅ: 339180
- ×¢²á: 2007-04-06
- רҵ: Í¬Î»ËØµØÇò»¯Ñ§
¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï
wbaishi(½ð±Ò+2,VIP+0):ллÈÈÇéÓ¦Öú£¡
hbqouc(½ð±Ò+5,VIP+0):·Ç³£¸Ðл
wbaishi(½ð±Ò+2,VIP+0):ллÈÈÇéÓ¦Öú£¡
hbqouc(½ð±Ò+5,VIP+0):·Ç³£¸Ðл
|
ÒѾ°ïÄãÏÂÔØ£¬Çë¼ûÁ´½Ó http://www.namipan.com/d/Global% ... ecc0a374781a0441c00 |

2Â¥2008-12-25 02:36:12
hbqouc
ľ³æ (ÖªÃû×÷¼Ò)
- Ó¦Öú: 38 (СѧÉú)
- ½ð±Ò: 3312.7
- É¢½ð: 954
- ºì»¨: 6
- Ìû×Ó: 5269
- ÔÚÏß: 235Сʱ
- ³æºÅ: 553345
- ×¢²á: 2008-05-03
- ÐÔ±ð: GG
- רҵ: º£ÑóµØÖÊѧ

3Â¥2008-12-25 12:13:18
hellysir
Òø³æ (ÕýʽдÊÖ)
- Ó¦Öú: 6 (Ó×¶ùÔ°)
- ½ð±Ò: 347.1
- É¢½ð: 400
- ºì»¨: 1
- Ìû×Ó: 779
- ÔÚÏß: 41.3Сʱ
- ³æºÅ: 380173
- ×¢²á: 2007-05-23
- ÐÔ±ð: GG
- רҵ: º£ÑóµØÖÊѧ
¡ï
Сľ³æ(½ð±Ò+0.5):¸ø¸öºì°ü£¬Ð»Ð»»ØÌû½»Á÷
Сľ³æ(½ð±Ò+0.5):¸ø¸öºì°ü£¬Ð»Ð»»ØÌû½»Á÷
|
ÍÆ¼öÄã¼ÓÈëAGU£¬³ÉΪËûµÄ»áÔ±¡£Ñ§Éú£·ÃÀÔªµÄÄê·Ñ£¬·ÇѧÉú£²£°ÃÀÔªµÄÄê·Ñ¡£µ«ºÃ´¦¶à¶à¡£ÃÀ¹úºÍµØÖÊÓйصÄÅóÓѼ¸ºõÈËÈ˶¼ÊÇ»áÔ±¡£ |
4Â¥2009-07-24 05:08:48
hbqouc
ľ³æ (ÖªÃû×÷¼Ò)
- Ó¦Öú: 38 (СѧÉú)
- ½ð±Ò: 3312.7
- É¢½ð: 954
- ºì»¨: 6
- Ìû×Ó: 5269
- ÔÚÏß: 235Сʱ
- ³æºÅ: 553345
- ×¢²á: 2008-05-03
- ÐÔ±ð: GG
- רҵ: º£ÑóµØÖÊѧ

5Â¥2009-08-16 19:50:03














»Ø¸´´ËÂ¥