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135. On the Relation between the Cool Summer in the Northern Japan and the Average Solar Radiation Intensity Measured at the Surface of the Earth

机译：135.关于日本北部凉爽夏季的关系及地球表面测量的平均太阳辐射强度

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Hidetosi ARAKAWA;
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年度 1943
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1. On the Relation between the Cool Summer in Northern Japan and the Average Solar Radiation Intensity Measured at the Surface of the Earth [J] . H. ARAKAWA ournal of the Meteorological Society of Japan . 1944,第5期

机译：日本北部凉爽的夏季与在地表测得的平均太阳辐射强度之间的关系
2. Enhanced annual litterfall production due to spring solar radiation in cool-temperate mixed forests of northern Hokkaido, Japan [J] . Maricar M. AGUILOS, Kentaro TAKAGI, Hiroyuki TAKA.HASHI, 農業気象 . 2012,第4期

机译：在日本北海道北部的凉爽混交林中，由于春季太阳辐射，增加了每年的凋落物产量
3. Solar Radiation: Calculating the Average Integral Solar Radiation Flux On Semicylindrical Heat Receiver Surfaces [J] . N.R. Avezova Applied Solar Energy . 1999,第6期

机译：太阳辐射：计算半圆柱形受热器表面上的平均整体太阳辐射通量
4. Comparison of imagined and real behaviors in relation to active cooling methods under Japanese summer conditions [C] . M. Schweiker, M. Shukuya Air infiltration and ventilation centre conference;AIVC 2008 . 2011

机译：与日本夏季条件下主动降温方法相关的想象和实际行为比较
5. Study of the Condensation Performance of Composite Coating on Copper Surfaces for Use in Solar-powered Adsorption Cooling Systems [D] . Zhu, Longqian 2018

机译：太阳能吸附冷却系统中铜表面复合涂层的冷凝性能研究
6. Earths magnetosphere and outer radiation belt under sub-Alfvénic solar wind [O] . Noé Lugaz, Charles J. Farrugia, Chia-Lin Huang, -1

机译：亚Alfvénic太阳风下的地球磁层和外部辐射带
7. Enhanced annual litterfall production due to spring solar radiation in cool-temperate mixed forests of northern Hokkaido, Japan [O] . Maricar M. AGUILOS, Kentaro TAKAGI, Hiroyuki TAKAHASHI, 2012

机译：日本北海道北部凉爽温带混合森林中的春季太阳辐射，增强了年度落下产量
8. Solar Intensity and Intensity and Polarization of Sky Radiation for 347.0, 488.0 and 533.5 NM. At Selected Points Along the Sun's Vertical and Other Meridians Measured at 2818 M A.S.L [R] . Bener, P. 1970

机译：太阳强度和强度与天空辐射极化分别为347.0,488.0和533.5 Nm。沿着太阳的垂直和其他经络的选定点测量到2818 m a.s.L.

135. On the Relation between the Cool Summer in the Northern Japan and the Average Solar Radiation Intensity Measured at the Surface of the Earth

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