Records of Production Rate in the Little Ice Age of Cosmic Ray Product 32Si in Arctic Ice Cores
スポンサーリンク
概要
- 論文の詳細を見る
Solar change, if it exists, must affect terrestrial climatic change. Recent observations of the total flux of solar radiation and the sunspot number have demonstrated the constancy of the sun. Therefore, the relation to solar change of climatic change should be investigated by using longer records. The change of production rate of the cosmic ray products in the earth's atmosphere is known to be useful as a measure of solar activity. Then, records indicating the production rates of ^<14>C and ^<32>SSi) in the atmosphere were investigated, especially in the Maunder Minimum, the period 1645-1715 A. D. in which almost no sunspots are considered to have occurred. The de Vries Peak, a prominent peak in the atmospheric ^<14>C concentration, is in remarkable agreement in sense and date with the Maunder Minimum. Nevertheless, the records indicating that the ^<32>(Si) production rate shows a trough in the Maunder Minimum was found in Arctic ice cores. This discrepancy found, if true, raises a doubt on the existence of the Maunder Minimum. Factors which might cause this discrepancy are discussed.
- 国立極地研究所の論文
- 1981-10-00
著者
-
Kato Kikuo
Water Research Institute, Nagoya University
-
Kato Kikuo
Water Research Institute Nagoya University
関連論文
- Oxygen isotopic composition of fallen snow in 1977 at Syowa Station, East Antarctica (extended abstract)
- Some Results on Oxygen Isotope and Stratigraphic Analyses of Firn in Mizuho Plateau, East Antarctica
- Rate of Snow Accumulation Determined from Oxygen Isotope and Stratigraphic Analyses of the Core from Mizuho Station, East Antarctica (Extended Abstract)
- Stratigraphic Analysis of Firn and Ice at Mizuho Station
- Oxygen isotope profile in the 150m core from Mizuho Station, East Antarctica (abstract)
- Oxygen Isotope Profiles in Adjacent Cores from Mizuho Station, East Antarctica
- Salt error in colorimetric determination of the molybdate-reactive silica in sea water
- Seasonal variation of oxygen isotopic composition of drifting snow at Mizuho Station, East Antarctica (abstract)
- Dilution and Concentration of Saline Water in Don Juan Pond in 1974
- CHEMICAL AND ISOTOPIC CHARACTERISTICS OF ICE FROM AN ICE-WEDGE IN SEYMOUR ISLAND (ISLA VCOM. MARAMBIO), ANTARCTIC PENINSULA REGION (II)
- Variations of oxygen isotopic composition and distribution of continental ice in the last ice age. (II) Massive ground ice body in Arctic Canada (abstract)
- CHEMICAL CHARACTERISTICS AND SALT ORIGIN OF THE WATER IN LAKE VANDA, WRIGHT VALLEY, SOUTHERN VICTORIA LAND, ANTARCTICA
- CHEMICAL AND ISOTOPIC CHARACTERISTICS OF ICE FROM AN ICE-WEDGE IN SEYMOUR ISLAND (ISLA VCOM. MARAMBIO), ANTARCTIC PENINSULA REGION (I)
- Chemical and isotopic characteristics of ice from an ice-wedge in Seymour Island (Isla Vcom. Marambio), Antarctic Peninsula region (I)
- Oxygen isotopic composition gross β-radioactivity in firn(Glaciology 4)
- VARIATIONS OF OXYGEN ISOTOPIC COMPOSITION AND DISTRIBUTION OF CONTINENTAL ICE IN THE LAST ICE AGE (III)
- Correlation between the monthly means of surface air temperature and oxygen isotopic composition of fallen snow at Syowa Station (extended abstract)
- Relationship between annual means of δ18O in cores from Mizuho Plateau and air temperature at Syowa Station, Antarctica (abstract)
- Correlation between snow accumulation rate on Mizuho Plateau and air temperature at Syowa Station, Antarctica (abstract)
- VARIATIONS OF OXYGEN ISOTOPIC COMPOSITION AND DISTRIBUTION OF CONTINENTAL ICE IN THE LAST ICE AGE. (II) MASSIVE GROUND ICE BODY IN ARCTIC CANADA
- Oxygen isotopic composition and formation process of snow under anti-cyclone at Syowa Station, East Antarctica (extended abstract)
- Records of Production Rate in the Little Ice Age of Cosmic Ray Product 32Si in Arctic Ice Cores
- Oxygen Isotopic Composition and Temperature of Formation of Fallen Snow in Antarctica
- Oxygen isotope profiles in the cores from Mizuho Station, East Antarctica and their climatic implications (abstract)
- VARIATIONS OF OXYGEN ISOTOPIC COMPOSITION AND DISTRIBUTION OF CONTINENTAL ICE IN THE LAST ICE AGE (I)
- IV. OXYGEN ISOTOPIC COMPOSITION AND GROSS 示篠-RADIOACTIVITY IN FIRN