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Loyal to the highest constituted power in the land, actuated by an innate love of rectitude his aims would be the strict maintenance of public order, the repression of many abuses though not of all simultaneously (every measure of reform or retrenchment being a preliminary solution to be contained by fluxion in the final solution), the upholding of the letter of the law (common, statute and law merchant) against all traversers in covin and trespassers acting in contravention of bylaws and regulations, all resuscitators (by trespass and petty larceny of kindlings) of venville rights, obsolete by desuetude, all orotund instigators of international persecution, all perpetuators of international animosities, all menial molestors of domestic conviviality, all recalcitrant violators of domestic connubiality.

在对本国的最高宪法所规定的国家最高权力的一片忠诚和与生俱来的正义感的驱使之下,他所追求的目标就是严格地维护社会秩序,扫除各种弊端,然而并非齐头并进(每一项改革或紧缩措施都是初步的解决,经过融化吸收,导致最后的解决)。对一切串通起来进行抗辩者,一切条例和规章的违反者,一切试图恢复已废止并失效的文维尔权者,国际间一切迫害的高声煽动者,国际间一切仇恨的鼓吹者,一切对家庭欢聚的卑鄙的破坏者,一切对夫妻关系死不悔改的亵渎者,要严格执行一切法律条文。

D its lonely hours and dreary, When we Close the aching sight, Musing sadly, lorn and weary, Trusting that tomorrow's light May reveal a day more cheery; Amid affliction's darker hour, When no hope beguiles our sadness, When Death's hurtling tempests lower, And forever shroud our gladness, While Grief's unrelenting power Goads our stricken hearts to madness; When from friends beloved we're parted, And from scenes our spirits love, And are driven, broken-hearted, O'er a heartless world to rove; When the woes by which we've smarted, Vainly seek to melt or move; When we trust and are deluded, When we love and are denied, When the schemes o'er which we brooded Burst like mist on mountain's side, And, from every hope excluded, We in dark despair abide; Then, and ever, God sustains us, He whose eye no slumber knows, Who controls each throb that pains us, And in mercy sends our woes, And by love severe constrains us To avoid eternal throes.

小时的孤独和凄凉,当我们关闭疼痛视觉,沉思可悲的是,洛恩和厌倦,相信明天的光线可能揭示出一个更愉快的一天;一片痛苦的黑暗时刻,当我们不希望翻滚的波涛上面悲伤,当死亡的飞驰暴风雨低,我们永远裹尸布高兴,虽然悲伤的不懈动力Goads我们灾区的心以疯狂;当从我们可爱的朋友分手,从场面我们的精神的爱,并驱动,伤心,O'er是无情世界的罗夫,当其中我们元气疾苦,妄想寻求融化或移动,当我们的信任和迷惑,当我们爱和被剥夺,当计划o'er 像我们反复思量山区一边薄雾破灭,从每一个希望排除,我们在黑暗的绝望遵守,那么,和以往任何时候都维持我们的上帝,他的眼睛没有沉睡知道,谁控制每一个跳动的痛苦我们,在我们的困境发出慈悲,爱和严重制约我们避免永恒的阵痛。

Miss you The Legend of Summer Night Is just the beginning of a beautiful Mature in autumn Should be followed Silently waiting Echo from afar Quietly miss you Like every day like its own Snow I like snow Like snow white Snow's arrogance To see snow fly Have been infatuated with snow Sentimentally attached to love Snow Snow In order to wait for the arrival of snow Hard守侯 Served snow dance song To write the text for the snow contest I love that vast expanse of whiteness of the snow Dance in the open wilderness where It's as charming dance I want to kiss drunk She is so fragile Melt in our hands It is so reluctant to produce water-based Although the cold outside It is still in its sky, fly It belongs to the cold northern land of Dream Away a sincere friend, I am wandering the streets at the shore, Do not know the destination where River, such as scales, and the roads were rare.

嗯,这次考试的题目是写一首英文诗歌,不会写呢,找了几篇帮忙翻译下吧~~拜托啦~~~如果有好的英文诗歌的话也可以写上来哦,不过前提是,一定要原创的呢~这些是我找的诗歌:(帮忙翻译成英文的哦~~)想你夏夜的传说只是美丽的开始成熟的秋季应该会接踵而至默默地等待来自远方的回音静静地想你就像每天想自己雪我喜欢雪喜欢雪的洁白雪的傲气看雪花飞舞曾迷恋雪眷恋雪钟情雪为了等待雪的到来苦苦守侯曾为雪歌唱起舞为雪写文比武我喜欢那白茫茫的雪花在空旷的原野里起舞它的舞姿那样妩媚让我陶醉想亲吻她是那么的娇弱捧在手中融化不愿意它那样化生成水虽然外面寒冷依然让它在它的天空飞舞它属于北国寒冷的国土追梦送走了真挚的朋友,我徘徊在岸边街头,不知道该去向哪里,河水如鳞、路上人稀。

According to the energy conservation theory, BOM and CSIM4 were coupled. The BOM has no treatment on transmission solar radiation, which is of great importance when the model is adapted to Arctic Ocean. So the treatment was introduced to BOM. Through numerical test on different lead albedos, it was found that sea ice thickness is not so sensitive to lead albedo, which may be contribute to the lead occupies little ratio within multiyear sea ice pack. The reason of summer over-melt of arctic sea ice is the NCEP reanalysis downward solar radiation being larger than its reality. Then the arctic sea ice climate variability was simulated. Results showed that: simulated ice thickness change is in accord with the submarine investigated mean sea-ice draft changes. Simulated annually maximum ice thickness along the Eurasian continental oceans are closely related to the observed ones. The long-term mean simulated ice motion has the same features of the SSM/I derived ice motion. Sea ice extents in differential sub-regions have same trends comparing to the satellite passive-microwave data derived ones. Simulated ice concentration is closely related to the observed in the Arctic sub-regions. Sea ice flux through the Fram Strait involves ice concentration, motion and thickness. It is a composite criterion for sea ice model evaluation. The simulated ice area and volume export through the strait accord with the satellite derived or statistically reconstructed ones.(5) The simulated ice thickness climate variability and mean sea surface current of the coupled model were analyzed, results showed: the total ice volume in the Arctic Ocean has a significant decreasing trend. The volume variability is of a 10-year timescale oscillation, with two major periods of 12-13a and 18-20a. Mean ice thickness in the arctic sub-seas has different tendencies. It has an increasing trend in the Barents-Kara Sea and Baffin Bay-Labrador Sea, and decreasing in the others. The characteristic time scale of 7-10a wherein the river discharges leads the Fram Strait ice volume export is about the period that river water takes to be conveyed across the Arctic Ocean.(6) Using the simulated ice distribution in the Arctic Ocean and China precipitation, air temperature and SST in tropical key regions, the climate teleconnection were studied. Result showed: When the mean sea ice thickness is large in the central Arctic Ocean and Chukchi-Beaufort Sea , and small in the Barents-Kara Sea and Baffin Bay-Labrador Sea , the precipitation in South China, Tibetan Plateau, and the north part of Northeastern China are always smaller than normal, and v. v. When the mean ice thickness is small in CA, BC, East Siberian Sea and Greenland-Iceland-Norwegian Sea , and large in BL, The air temperature in north-eastern China, the southern of Tibetan Plateau, and Hainan Island, are always lower than normal, and v. v. In addition, when the sea ice is thick in BC and BL, the SST is larger in the middle and eastern Pacific Ocean, and is smaller in the tropical Southeastern Indian Ocean.

由于BOM没有考虑透射太阳辐射的物理过程,研究表明透射太阳辐射对北冰洋的能量收支起到重要作用,因此在BOM模式中引入了对透射太阳辐射的处理;通过对不同水道反照率的数值试验表明海冰厚度对水道反照率的敏感性不强,可能与海冰区水道面积占的比率很小有关;而模式模拟的北极海冰夏季&过度融化&主要源于NCEP再分析资料提供了偏大的太阳短波辐射;对北极海冰的气候变率进行了模拟研究,结果表明:模拟的海冰厚度变化与潜艇探测的海冰吃深度变化具有一致性;模拟和观测的亚欧大陆沿海的年内最大海冰厚度有很好的相关;模拟的海冰移速与长期平均的卫星反演的海冰移速具有相同的速度分布特征;模拟的各个海区海冰面积的变化趋势与卫星反演资料分析的结果基本一致;模拟与观测的主要海洋分区的海冰密集度具有很好的相关:弗瑞姆海峡的海冰体积和面积的输送涉及到海冰密集度、厚度和移动速度,是判断模式模拟能力的一个综合的指标,模式模拟的结果与卫星反演或重建的面积输送、体积输送具有很好的一致性;(5)分析了模拟的北极海冰厚度的气候变率及气候平均表层海流场,结果表明:北极海冰的总体积有显著减少的趋势,北极海冰总体积的变化具有10a际尺度振荡的特点,存在18-20a和12-13a两个主周期;北极海冰的平均厚度在各个海区的变化趋势不同,在巴伦支—喀拉海和巴芬湾—拉布拉多海地区海冰厚度有显著的增加趋势,而其它海区存在减少的趋势;通过对模拟的气候平均表层海流的分析表明,北极河流流量超前弗瑞姆海峡海冰流量7-10年的特征时间尺度与表层海流的气候分布存在着必然联系:(6)利用模拟结果以及中国降水、气温和热带关键区SST资料,讨论了北极各海区海冰平均厚度与中国降水、气温以及热带关键区SST的关系,结果表明:在北极中心海区和楚科奇—波弗特海海冰厚度偏大,在巴伦支—喀拉海以及巴芬湾—拉布拉多海海冰厚度偏小,则中国降水在华南地区、青藏高原和东北北部降水偏少,反之相反;在北极中心海区、东西伯利亚海、楚科奇—波弗特海以及格陵兰海海冰厚度偏小,在巴芬湾—拉布拉多海海冰厚度偏大,则在中国东北地区、高原南部地区和海南岛附近气温偏低,反之相反;另外,北极楚科奇—波弗特海和巴芬湾—拉布拉多海海冰厚度偏大时,在热带中东太平洋海温偏高,而在热带东南印度洋海温偏低。

John Cena In case you forgot or fell off I'm still hot - knock your shell off My money stack fat plus I can't turn the swell off The franchise, doin big bid'ness, I live this It's automatic I win this - oh you hear those horns, you finished A soldier, and I stay under you fightin Plus I'm stormin on you chumps like I'm thunder and lightning Ain't no way you breakin me kid, I'm harder than nails Plus I keep it on lock, like I'm part of the jail I'm slaughterin stale, competition, I got the whole block wishin they could run with my division but they gone fishin -- with no bait, kid your boy hold weight I got my soul straight, I brush your mouth like Colgate In any weather I'm never better your boy's so hot you'll never catch me in the next man's sweater If they hate, let 'em hate, I drop ya whole clan Lay yo' ass DOWN for the three second TAN Yeah, uhh It's gon' be what it's gon' be Five pounds of courage buddy, bass tint pants with a gold T Uhh - it's a war dance and victory step A raw stance is a gift, when you insist it's my rep John Cena, Trademarc, y'all are so-so And talk about the bread you make but don't know the recipe for dough though Aimin guns in all your photos, that's a no-no When this pop, you'll liplock, your big talk's a blatant no-show See what happens when the ice age melt You see monetary status is not what matters, but it helps I rock a timepiece by Benny if any The same reason y'all could love me is the same reason y'all condemn me A man's measured by the way that he thinks Not clothing lines, ice links, leather and minks I spent 20 plus years seekin knowledge of self So for now Marc Predka's livin live for wealth

约翰Cena 如果你忘了或掉了我仍然热-敲你的shell关闭我的钱堆脂肪加上我不能把膨胀关闭此外,该公司的乐队大bid'ness ,我住这它的自动我赢了这一点-哦你听到那些喇叭,你完成一名士兵,我留你的领导下fightin 加上我stormin你chumps像我雷电不是没有办法你分手我的孩子,我比指甲加上我一直就锁,想我的一部分,监狱我slaughterin陈旧,竞争,我得到了整个块wishin 他们就可以与我司,但他们已经fishin --没有诱饵,孩子的体重男孩举行我得到了我的灵魂直,我刷你的嘴像高露洁在任何天气条件下我从来没有更好的男孩这么热你将永远不会赶上我在接下来的男子的毛衣如果他们的仇恨,让'时间的仇恨,我下拉亚整个家族躺在你'屁股下跌三秒谭是啊, uhh 这是坤'是它的坤'是 5磅的勇气好友,低音色彩裤与黄金 Uhh -这是一个战争舞蹈和胜利的一步原材料的立场是一个礼物,当你坚持这是我的代表约翰Cena , Trademarc ,你们是马马虎虎谈论你的面包,但不知道的良方面团虽然爱民枪在您的所有照片,这是一个没有任何当此弹出,您liplock ,您的大Talk的公然没有出现看看会发生什么时,融化冰河时代你看到的货币地位没有什么问题,但它可以帮助余岩计时器的班尼如有由于同样的原因你们可以爱我是同样的原因你们谴责箱一个人的方式来衡量的,他认为没有衣物线,冰链,皮革和水貂我花了20余年seekin知识的自我因此,现在马克Predka的生存生活的财富完全直译过来的主要没看过这比赛没语感没法意译

Based on the data analysis and numerical simulation, the Arctic sea ice climate variability was researched, the result were as following:(1) The analysis on the seasonal cycle of the Arctic Ocean and atmosphere showed that: The seasonal surface wind is somewhat trade wind like in some regions in the Arctic. The surface air temperature is robustly determined from the underlying environments such as sea ice and Greenland glaciers. In the sea ice region the precipitation rate is larger than that of evaporation. Furthermore, the Arctic Ocean hydrology is profoundly influenced by the surrounding rivers discharge. These are the decisive factors on the ocean salinity pattern. Sea ice flux through the Fram Strait is larger in winter than in summer. From the 40s in the 20th century on, the ice volume flux has an increasing trend. The Arctic rivers flood season is about the melt period, the winter rivers discharge has a significant increasing. Correlation analysis shows that 7 to 10 years is a characteristic time scale that rivers discharge leads Fram Strait ice volume export.(2) Considering 9 major arctic rivers, the Arctic Ocean circulation was simulated through BOM. The result shows that: The BOM can reproduce the main Arctic Ocean circulation pattern. The"Islandization"which is commonly used in OGCMs to treat the North Pole, not only influences the ocean current near the pole, but also influences the current in the Northern Atlantic Ocean, thus the bogus island might influence global climate through thermohaline circulation in the Atlantic Ocean.

在资料分析和数值模拟的基础上,对北极海冰的气候变率进行了深入的研究,结果如下:(1)对北极地区大气和海洋季节循环特征的分析表明,气候平均风场在部分地区具有&信风&的性质;而气温场与海冰分布及格陵兰半岛冰原的下垫面特征有密切关系;在北极海冰区的降水量大于蒸发量,并且在全球大洋中北冰洋受到河流径流的影响最大,对北冰洋的盐度分布有决定作用;通过弗瑞姆海峡的海冰通量在冬半年大于夏半年,并且从20世纪40年代起,海冰的体积输送有增加趋势;北极河流的汛期主要在融化季节,冬季的河流流量有显著增加的趋势;相关分析表明7到10年是北极河流流量影响弗瑞姆海峡海冰体积输送的一个特征时间尺度;(2)采用BOM海洋模式对北冰洋海洋环流进行了模拟研究,在模式中考虑了北极9条主要河流的作用,结果表明该海洋模式可以较好模拟出北冰洋海洋环流的基本特征;多数大洋环流模式采用&北极岛化&的方法处理北极点,模拟结果表明&北极岛化&不仅影响到极点附近的海流,还会对相对较远的北大西洋海流造成影响,并可能通过大西洋的热盐环流对全球气候产生影响;(3)采用CSIM4海冰模式对北极海冰的气候态进行了模拟。

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