Fred H Skogseth
Dados Biográficos
| ID | 5597155 |
|---|---|
| NOME | Fred H Skogseth |
| PRENOMES | Fred H |
| SOBRENOME | Skogseth |
| ASSINATURA | SKOGSETH F H |
| VERIFICADO | Não |
| TOTAL DE OBRAS | 2 |
| TOTAL DE CITAÇÕES | 13 |
| TOTAL COMO AUTOR | 2 |
| TOTAL COMO EDITOR | 0 |
| PRIMEIRO ANO DE PUBLICAÇÃO | 1980 |
| ANO MAIS RECENTE DE PUBLICAÇÃO | 1984 |
| ÍNDICE H | 2 |
Bomb 14 C in the Ocean Surface 1966–1981
Bomb 14 C has been used as a tracer for CO 2 in ocean surface water to study CO 2 exchange between atmosphere and ocean. Using ordinary cargo ships for sampling, we have been able to cover some parts of the Atlantic, Pacific, and Indian Oceans for certain periods. A total number of 520 samples from 89 locations were measured during the last 15 years. The data are presented both in tables and graphs. A maximum 14 C concentration (Δ 14 C) of ca 20%…
Transfer of Bomb 14 C to the Ocean Surface
Additional 14 C data from the atmosphere and ocean have been provided since the ninth 14 C conference in 1976. At the moment, one sampling station in the troposphere in each hemisphere seems to give sufficient accuracy for exchange studies. The 14 C concentration in the troposphere in December 1978 constituted a mean value of 30 ± 1 percent (Δ 14 C) above normal level, a concentration that has been reduced to about one half during 12 years. 14 C …
Bomb 14 C in the Ocean Surface 1966–1981
Bomb 14 C has been used as a tracer for CO 2 in ocean surface water to study CO 2 exchange between atmosphere and ocean. Using ordinary cargo ships for sampling, we have been able to cover some parts of the Atlantic, Pacific, and Indian Oceans for certain periods. A total number of 520 samples from 89 locations were measured during the last 15 years. The data are presented both in tables and graphs. A maximum 14 C concentration (Δ 14 C) of ca 20%…
Transfer of Bomb 14 C to the Ocean Surface
Additional 14 C data from the atmosphere and ocean have been provided since the ninth 14 C conference in 1976. At the moment, one sampling station in the troposphere in each hemisphere seems to give sufficient accuracy for exchange studies. The 14 C concentration in the troposphere in December 1978 constituted a mean value of 30 ± 1 percent (Δ 14 C) above normal level, a concentration that has been reduced to about one half during 12 years. 14 C …
Transfer of Bomb 14 C to the Ocean Surface
Additional 14 C data from the atmosphere and ocean have been provided since the ninth 14 C conference in 1976. At the moment, one sampling station in the troposphere in each hemisphere seems to give sufficient accuracy for exchange studies. The 14 C concentration in the troposphere in December 1978 constituted a mean value of 30 ± 1 percent (Δ 14 C) above normal level, a concentration that has been reduced to about one half during 12 years. 14 C …
Bomb 14 C in the Ocean Surface 1966–1981
Bomb 14 C has been used as a tracer for CO 2 in ocean surface water to study CO 2 exchange between atmosphere and ocean. Using ordinary cargo ships for sampling, we have been able to cover some parts of the Atlantic, Pacific, and Indian Oceans for certain periods. A total number of 520 samples from 89 locations were measured during the last 15 years. The data are presented both in tables and graphs. A maximum 14 C concentration (Δ 14 C) of ca 20%…
Atmospheric sciences (2 obras) · Climatology (2 obras) · Environmental Science (2 obras) · Geography (2 obras) · Geology (2 obras) · Meteorology (2 obras) · Oceanography (2 obras) · Atmospheric and Environmental Gas Dynamics (1 obras) · Atmospheric chemistry and aerosols (1 obras) · Chemistry (1 obras)