何锐 @[email protected]

«想死 12»

我不说不代表我不想死，
在我沉默的时候更会想。
这件事不用告知任何人，
不再统计一天想多少次。

«英雄母亲»

Born to be 人口红利
Born to be 精神疾病
Born to be 铁链
Born to be 英雄母亲

April 13th
Neptune, spotted in 1989 from NASA’s Voyager 2 spacecraft.
THE ICE GIANT NEPTUNE is the furthest known planet in our solar system, and has an atmosphere composed largely of hydrogen and helium. Neptune also has vast streaks of cloud that consist of frozen methane and ammonia. From space, Neptune’s atmosphere appears quite serene, thanks to its bright blue color. It is, however, anything but calm. The Great Dark Spot in the center of this image is an enormous storm system extending the width of Earth that swirls around the planet, creating winds of 2,100 kilometers per hour (1,300 miles per hour). The isolated white patch appearing here a little below the Great Dark Spot is a region of cloud dubbed the “Scooter.” This is because the persistent cloud feature rotates faster around the planet, lapping the Dark Spot every 12 rotations. The calm-looking Neptune turns out to have some of the strongest winds in the whole of our solar system.
海王星，被观测于 1989 ，来自美国国家航空航天局的旅行者 2 号太空飞行器。
海王星这冰巨星在我们的太阳系的行星中是已知最远的，有一个大部分是氢和氦组成的大气。海王星也有着成份是冰冻甲烷和氨气的广袤的云的条斑。从太空看，海王星的大气显得相当宁静，得归功于它的明亮的蓝颜色。可它就是不平静。在这个影像中心的大暗斑是个硕大的风暴系统，广达地球之宽并绕着海王星旋转，造出每小时 2100 千米（每小时 1300 英里）的风。此处在大暗斑下方一点现出的孤立的白色补缀是一个外号「滑板车」的云区。这是因为特征坚挺的云绕着行星转动得更快，每 12 转就会搭在暗斑上。看似平静的海王星可想而知有着一些在我们的整个太阳系中最强的风。

April 12th
A traveling volutus, or roll cloud, spotted by Jean Louis Drye as it sweeps over his cargo ship off the coast of São Paulo, Brazil.
ROLL CLOUDS, KNOWN OFFICIALLY AS VOLUTUS, form within a traveling wave of air. One can sometimes travel ahead of an advancing storm, but it is more commonly produced by the interaction of sea breezes. This is why roll clouds tend to be spotted over coastal waters. The rising air at the front of the wave and the dipping air at the back are not visible, just the rotating roll of cloud in the middle, but they can be felt as shifting air currents. “There was a sudden strong wind,” reported Jean Louis Drye, who spotted the formation, “just as the cloud was passing over.”
行进中的滚卷云，或称翻滚云，被 Jean Louis Drye 观测到它扫过他的驶离巴西圣保罗的海岸的货船上空。
翻滚云，正式名称为滚卷云，形成于一股行进的气浪之中。有时会有个可以在前进的风暴的前头行进，但它还是更常被海风的相互作用所制造。这就是为什么翻滚云趋于在近岸水体上空被观测到。在气浪的前面的上升气流和在背面的下浸气流不是可见的，只有在当中转动的云卷，但它们可以因着变换的气流被感觉到。「有一阵突然的强风，」 观测到该形体的 Jean Louis Drye 报道，「就在这云刚经过时。」

April 8th
A sunset of Cumulus, Cirrus, and Cirrus floccus clouds provides the backdrop as NASA’s Cygnus spacecraft approaches the International Space Station for docking. The craft, photographed by ISS flight engineer Thomas Pesquet, is carrying supplies for the crew and equipment for their experiments.
一次日落，积云、卷云、絮状卷云充当了美国国家航空航天局的天鹅座号宇宙飞船对接国际空间站以入坞时的背景。该飞行器，被国际空间站飞行工程师 Thomas Pesquet 拍摄到，正在运载给工作组的补给品和他们的实验设备。

April 9th
Cloud Gate (2004), a public sculpture created by Indian-born British artist Sir Anish Kapoor in Millennium Park, Chicago, US, shines beneath Cirrus, a high cloud created by ice crystals cascading from the upper reaches of the troposphere.
云彩之门（2004），一座公共雕塑，由生于印度的不列颠艺术家 Anish Kapoor 爵士创作于美国芝加哥的千禧年公园，在卷云之下闪耀——一种由冰晶从对流层的较高区域倾泻而下所创造的高云。

April 10th
Stratus, spotted by Filip Gavanski over the Roppongi district of Tokyo, Japan.
A BUILDING WITH ITS HEAD IN THE CLOUDS is in the grey, featureless world of the Stratus cloud. Stratus is the lowest of the ten main cloud types. Though beautiful when viewed from above, it can feel close, even oppressive, from below. When it forms down at ground level Stratus is known as fog or mist, but up at 450 meters (1,500 feet) where it often lurks, it is the sky that skyscrapers scrape.
层云，被 Filip Gavanski 观测于日本东京的六本木街区上空。
一座云里雾里的建筑处于灰暗，毫无特色的层云的世界中。层云是十大云类中最低的。虽然从上方下看的时候会美，从下方上看会感觉很近甚至有压迫感。当它形成降至地面水平，层云被人称作雾或霭，但是上至 450 米（1500 英尺）它经常潜伏之处，那天空就是摩天大楼的刮痕。

April 11th
A Stratocumulus sunset at lunchtime. Spotted in the middle of the day over Great Salt Lake, Utah, US, by Jeremy Hanks (Member 41,507).
WE ARE USED TO SEEING CLOUDS turn pink at the beginning and the close of day as they reflect the rosy hues of the low Sun. But this Stratocumulus cloud over Utah, US, appeared pink at 1.00 pm. What on Earth could cause clouds to be colored like this at lunchtime? The cause is indeed found on Earth. The pink patch on the cloud’s underside is a reflection of the Great Salt Lake below. Its waters can develop a distinctly reddish hue due to the salt-loving bacteria that thrive in its highly saline environment. They are tiny microbes with the power to summon sunsets in the middle of the day.
午餐时间的层积云霞。在一天的正中被观测于美国犹他州大盐湖上空，来自 Jeremy Hanks (赏云学会成员 41,507)。
我们惯于看着云彩在一天的开端和闭幕时转粉，因着它们反射低角度太阳的玫瑰般的色调。但是这个美国犹他州上空的层积云云彩，在午后一点钟显现了粉色。地球上的什么能使得云彩在午餐时间像这样被着色？原因的确要在地上找。在云彩的底面上的粉色补缀是下方的大盐湖的一个映照。它的水体可以由嗜盐细菌在它的高盐环境中繁盛而发展成显著的泛红色调。它们这些细小的微生物有能于在一天的正中召唤晚霞。

«梦魇»

被发现它已经转移或者再也不见，
所有迹象在同一条路上消逝干净。
接受和记忆所推导的不同的结局，
这些光亮起之前必须受难于黑夜。

«余»

小时候害怕摇滚歌手预言的彻底孤独，
虽然已经很孤立但仍然觉得可以改变，
后来逐渐发现不愿落单就免不了吸毒。
生态恶劣的时候能茕茕孑立反而幸运，
该担心丧失独善其身的意志走入歧路,
只不过路径本身就只有一条没有其他。
动摇和摆荡后终会回归引力所向之处，
原来那些努力标榜个性和包装自己的
也不过是又一些去迎合的流行和谬误。
权欲无有名利无求不逐财死不随人流，
不需要你不需要他不需要努力做个我，
问我活着干什么我说喜欢自己是多余。
有一件事最好尽快学会那就是尝出来
酸涩味道的多余等于正在生长的自由。

April 7th
Pileus on top of Cumulus congestus, spotted by Jaap van den Biesen and Nienke Edelenbosch over Nkhata Bay, Malawi.
THESE TWO CLOUD CAPS, known as pileus, developed in Malawi over the top of Cumulus congestus clouds that were well on their way to maturing into Cumulonimbus storm clouds. Pileus can appear as airstreams overhead that are lifted by the Cumulus’s rising convection currents, which can be extremely powerful in the tropics. The delicate-looking caps are like lenticularis or mountain cap clouds that have formed not over mountainous terrain but mountains of Cumulus. Droplets form where the airflow lifts and cools, only to evaporate away again as it sinks back down and warms beyond the cloudy obstacle. Being so short-lived, the droplets tend to be small and even in size—perfect for diffracting the sunlight and separating it into pearlescent colors. These can be just visible if you look carefully. Clearly, not every cloud has a silver lining. Some clouds have subtle multicolored ones.
幞帽盖在浓积云的顶上，由 Jaap van den Biesen 和 Nienke Edelenbosch 观测于马拉维的恩卡塔贝。
这两个云的盖帽，人称 Pileus (是古希腊和罗马人穿戴的一种无檐毡帽，即幞状云)，成体在马拉维上空浓积云云彩的顶部，恰是应了它们成熟变作成积雨云风暴云彩的过程。幞状云的出现可以是因空中的气流被积云里的上升对流所抬升，这在热带可以变得极其有力。这些外观精致的盖帽就像荚状云或山帽云彩不过并非形成在多山的地势上空而是积云的山上。液滴形成在气流抬升而冷却之处，只有在它下沉回落超越云的阻碍回暖时会再次蒸发掉。这么短命的，液滴趋于变作小小的甚至是完美适于衍射太阳光线并把它分离成珠光宝气的色彩。这些都可以看出来，如果你仔细地瞧。清楚的是，不是每朵云都有银色内衬。有的云有隐约多彩的一个。

April 6th
Altocumulus perlucidus, spotted over Mount Fuji, Japan, in around 1830 by Katsushika Hokusai.
WHEN THE CLOUDLETS in a layer of mid-level Altocumulus have gaps between them like this, they are described as perlucidus. This print by the 19th-century Japanese artist Katsushika Hokusai is from his classic series Thirty-Six Views of Mount Fuji. It is titled South Wind, Clear Sky (Gaifū kaisei). That strikes us as a bit of a misnomer.
高积漏隙云，被观测于日本富士山上空，在 1830 左右由葛饰北斋。
当一层中等水平高积云中的云块像这样在它们之间有豁口，它们就被描述为漏隙云。这副19世纪的日本艺术家葛饰北斋所作的版画，出自他的经典系列 «富岳三十六景»。它被定标题 «凯风快晴»。我们觉得有点用词不当。

April 4th
A parhelic circle and 120-degree parhelion caused by diamond dust, spotted by Richard Corrigall (Member 4,393) over La Plagne, France.
THE COLD WINTER AIR high in the French Alps is perfect for forming the glittering ice-crystal mist called diamond dust. When ice crystals grow slowly in drier conditions, they can form as tiny, clear, hexagonal prisms that bend and bounce sunlight to form all manner of curious spots and rings across the sky, known collectively as halo phenomena. The curved line of light appearing here is one such phenomenon, called a parhelic circle. It is a white band that runs parallel to the horizon, sometimes extending 360 degrees around the whole sky. It is always at the same height as the Sun, and tends to be a very fleeting effect. The bright spot appearing along the parhelic circle here is called a 120-degree parhelion. This is similar to a regular parhelion, known as a sun dog, but it is colorless, much further away from the Sun, and far less frequently spotted.
一个由钻石尘所致的幻日环和 120 度幻日，由 Richard Corrigall (由赏云学会成员 4,393) 于法兰西拉普拉捏上空观测到。
高在法国阿尔卑斯之端的寒冷冬季空气，完美适合形成被叫做钻石尘的莹莹烁烁的冰晶雾。当冰晶在较干的条件中缓慢成长，它们可以形成微小的、清晰的、六边形的棱柱，会弯折和弹射太阳光线形成天空之中形形色色稀奇的光斑和光环，它们被统称为光晕现象。此处显现出的光的弯曲的线条就是这么一种现象，被叫做幻日环。它是一条白色的带子，平行于天际线，有时延展到 360 度环绕整个天空。它总是与太阳处于同一高度，是趋于瞬逝的一种效应。此处随幻日环显现出的亮斑被叫做「120 度幻日」。这和一个常规的幻日是类似的，不过它没有颜色，离太阳更远得多，而且远没那么频繁的被观测到。

April 5th
Altocumulus castellanus, spotted over northwest Oregon, US, by Sallie Tisdale (Member 42,126).
THE CLOUD SPECIES known as castellanus is not the most distinctive of formations. In fact, it is easily missed, even by cloudspotters. But castellanus clouds like these spotted by Sallie Tisdale over Oregon, US, are worth looking out for because they often forecast storms later in the day. The cloud’s turrets indicate that the atmosphere up at the cloud level is unstable. When the crenellations of castellanus appear in Altocumulus clouds like these, they indicate that the unstable air is up at the mid-level of the clouds. This is significant. It suggests that any Cumulus clouds building from below as the day progresses will, upon reaching the unstable air, just keep growing. They’ll likely continue to develop taller and taller until they’ve matured into Cumulonimbus storm clouds. “The sky was active all day,” Sallie confirmed, “and that night we did indeed have thunderstorms.”
高积城堡云，被观测于美国俄勒冈西北部上空，来自 Sallie Tisdale (Member 42,126)。
人称城堡云的云种的形体并非是最鲜明的。其实，它是易于错会的，即便是观云者们。但像这些由 Sallie Tisdale 观测于美国俄勒冈上空的城堡云云彩值得留意，因为它们经常预示当天稍迟的暴风雨。云彩的塔楼指明了上至云层水平的大气是不稳定的。当城堡云的雉堞像这样出现在高积云云彩中，它们指明了不稳定的空气升过中层水平的云。这是意义重大的。这暗示着任何从下方筑起的积云随着一天的进展都会——往上达到不稳定的空气——只保持生长。它们很可能继续发育得越来越高直到他们已经成熟了变作积雨云的暴风雨云。「天空活跃了整日，」Sallie 证实了，「而那夜我们的确有了雷雨。」