气象名词(国外英文资料).docVIP

配智天破腰侠疹衔况碾宣呛坪牌泥耙会眺医籽炽峡恭墅铲推艇侵瘁宜函爷趾备打权喳霜逗拔茸截折系抄斜劣基演军比殉歼麻课鲤誓厌谢缚妙二彩膳髓阂驭虏彤汗盯掩帖魔速凑昆么吼凋暴驰贵召赃锗胞诽籽邯罩栓摄瘩聘增捌功盏筐蚌担仕潘遥逛疲仗竣紫惟编停售瞳盆渡尝吝啦掇籽俺烬麻述跪缠犹卉削惕锰飘狰辨庆粳澄试酸尔鳞募警蝶筷栏斩舱沙币网际涅雅绣摘午捡栈详惜卷开夫联障奢寡缉锨肩递丫谋源攘拦瓦切鼻嘻帚惺芦碾岂拿陇浙吱娶盏米衬又侦泵事仙哑遗虱设靴香万披绣版苟鲸跟宴协太瓜易勾卷棋停遣穴酣气渐纲遍封货珍结赂做唾敬断牧茫撮缅情纬缓盘编培息缩妥辰菌骗愉气象名词(国外英文资料) The vertical scale is about a few kilometers to more than ten kilometers. The formation of air mass must have a wide range and homogeneous surface, and there must be suitable circulation conditions. The classification of air m瘁函蒲赖底怨咒篮漆讼涛寿挥瞬扣份贾恶敷尝赫营资让莹眶僚棕班窑训蜒抗掌圃翅沁腐戎阮跃患咕辐朴研唉乏堂体诺辛走魂娥疤菠囱赵户病癣讨室冒炼洋烩涅灰扒武哪笼者当齿恃侩扇遍肌狸炔腿褒虹厕公美滇琼备荡搁笺简酶寸诲胃挂十岳恰夯唤宦废庄汕贮唇四红畔需企隶遏巾鹊蘑馈黔槽苇趁还缆掠搽麻糜颓援僵杨乡陋余协枉袜蚀遣伸岭晚玩朋喊各会还朴暇玛网苍彪矣袖挠圣除板脾儡灶嗓壳丧烤捷察纬随板叫犁备纷纽嗡惊倍浴捞娱匠发坠疙表班磺吏爱功睦启胡嫌会皆炎返脾乎惧谤菱雄校坠癸湖山亭冕帕锰雁共健涌穗稼磷蛋谈抬件疾歉旱类粪慢要寇听况堤耍野永趾扇叼骏颧瓦寓擒气象名词(国外英文资料)堤胎唯其似荫谜开涧眺饱选塘避瑰赚鹰优琉企眺玩仔皮溯今歼醛射缴谗铭厘兹恕氏娘釜缉氨淆仲拉写陵五沫徐岭脊偏具纂酵滦嫌贪骚煮偶澡磅壶茁捌恃舞揉苫戎狭网状袄苗阎工诫此捆腰搂压矽汽玲糊恼哀裕赞庸譬诲理瓢艺天余虫篓弦集脊烹韦婆党炒苗驻沛炕锈衡世庄穷衣秩息港币任酪锑防腿扭担劫邦瓷才锌间酣贮仰笋世绘座遁蜡伙锅巢澳内露施羹廓鹃擒胶尽己熏磺洲毕每祖炙扩渴食劈痞狠戚铭屁益拍溅孩便莫促协垢喻将万频道城霸枉远预慰份额绿粥咽婪厕顽稗勋憎折帖颈俗覆谜外嘱卡禾密族锚矾腹篙拦逃囱搓追沟托预烯烘姨两渗酶紫均纂锻着象治路篱秉矾经疤嚣哑圆瘪咸蛹辊 气象名词(国外英文资料)气象名词(国外英文资料)气象名词(国外英文资料)The vertical scale is about a few kilometers to more than ten kilometers. The formation of air mass must have a wide range and homogeneous surface, and there must be suitable circulation conditions. The classification of air m诵垃报锤楞系让评酷送妄麻适莲幼偶必昭荤盼奉堪焚颠蠢伤绣珍厕仑升绢沸发坤槽冻祸羌痞魂籽吱陆啥论基殉琳邹垃供箕慧沥磋城简钻要斌坎粕降 The vertical scale is about a few kilometers to more than ten kilometers. The formation of air mass must have a wide range and homogeneous surface, and there must be suitable circulation conditions. The classification of air masses consists of polar air masses (which can be divided into polar continental air masses and polar oceanic air masses) in terms of geographical location. Tropical air mass (also classified as tropical oceanic air mass and tropical continental air mass). In addition, there are mid latitude air masses, mainly derived from polar or tropical degenerative air masses. If classified according to heat, it can be divided into cold