锡林郭勒盟植被物候枯黄期对干湿变化的时间多尺度响应

基于全球监测与建模组(GIMMS)1982～2015年第三代归一化植被指数(NDVI)GIMMS NDVI 3g数据集和气象观测数据,采用累计NDVI的Logistic曲线曲率极值法提取锡林郭勒草原植被枯黄期,并结合不同时间尺度标准化降水蒸散指数(SPEI)分析植被枯黄期对干湿变化的响应特征.结果表明:1982～201...     

Analysis of Meteorological Drought Pattern During Different Climatic and Cropping Seasons in Bangladesh

Drought is one of the most frequent natural disasters in Bangladesh which severely affect agro‐based economy and people's livelihood in almost every year. Characterization of droughts in a systematic way is therefore critical in order to take necessary actions toward drought mitigation and sustainable development. In this study, standardized precipitation index is used to understand the spatial distribution of meteorological droughts during various climatic seasons such as premonsoon, monsoon, and winter seasons as well as cropping seasons such as Pre‐Kharif (March‐May), Kharif (May‐October), and Rabi (December‐February). Rainfall data collected from 29 rainfall gauge stations located in different parts of the country were used for a period of 50 years (1961‐2010). The study reveals that the spatial characteristics of droughts vary widely according to season. Premonsoon droughts are more frequent in the northwest, monsoon droughts mainly occur in the west and northwest, winter droughts in the west, and the Rabi and Kharif droughts are more frequent in the north and northwest of Bangladesh. It is expected that the findings of the study will support drought monitoring and mitigation activities in Bangladesh.     

酸性氯化铜蚀刻废液一步沉淀法制备碱式碳酸铜

以酸性氯化铜蚀刻废液为原料,在Na₂CO₃和助剂A存在下,采用一步沉淀法制备碱式碳酸铜。考察了反应pH、n（Na₂CO₃）∶n（助剂A）、反应时间和反应温度对碱式碳酸铜制备效果的影响,并采用XRD、TG 及SEM对产品进行了表征。实验结果表明：在反应pH 7.0、沉淀剂配比n（Na₂CO₃）∶n（助剂A）=1∶2、反应时间1.0 h、反应温度70 ℃的条件下,产品的w（Cu²⁺）达55.62%,w（Cl^-）为0.013%,符合HG/T 4825—2015《工业碱式碳酸铜》的要求;蚀刻废液中Cu²⁺的回收率接近100%。表征结果表明,制得的产品为单一组分CuCO₃·Cu（OH）₂,小颗粒为直径1.8~5.4 μm的不规则球形,团聚后的大颗粒呈姜块状形貌,粒径为48~75 μm。     

A multidecadal oscillation in precipitation and temperature series is pronounced in low flow series from Puget Sound streams

In Pacific Northwest streams, summer low flows limit water available to competing instream (salmon) and out-of-stream (human) uses, creating broad interest in how and why low flows are trending. Analyses that assumed linear (monotonic) change over the last ~60 years revealed declining low flow trends in minimally disturbed streams. Here, polynomials were used to model flow trends between 1929 and 2015. A multidecadal oscillation was observed in flows, which increased initially from the 1930s until the 1950s, declined until the 1990s, and then increased again. A similar oscillation was detected in precipitation series, and opposing oscillations in surface temperature, Pacific Decadal Oscillation, and Interdecadal Pacific Oscillation series. Multidecadal oscillations with similar periods to those described here are well known in climate indices. Fitted model terms were consistent with flow trends being influenced by at least two drivers, one oscillating and the other monotonic. Anthropogenic warming is a candidate driver for the monotonic decline, and variation in (internal) climatic circulation for the oscillating trend, but others were not ruled out. The recent upturn in streamflows suggests that anthropogenic warming has not been the dominant factor driving streamflow trends, at least until 2015. Climate projections based on simulations that omit drivers of multidecadal variation are likely to underestimate the range, and rate of change, of future climatic variation.     

塔城地区的干旱因素探讨

通过对塔城地区自然情况及水利设施建设方面的介绍及分析，总结了影响干旱的一些因素，并提出了相应的对策和建议，以减缓塔城地区的干旱问题。     

GPM卫星降水数据在天山山区的适用性分析

卫星降水产品在山区的适用性具有较高的不确定性。论文基于天山山区2014-2015年167个气象站点数据,应用较为广泛的两套卫星降水产品--TRMM与CMORPH,选用均方根误差（RMSE）、相关系数（R）、相对误差（PB）,以及分类统计分析指标（错报率FAR、探测率POD、公正先兆评分ETS、频率偏差BIAS）等,评估了新一代卫星降水产品--Global Precipitation Measurement（GPM）在天山山区的适用性。结果表明：相对于以上两种产品,GPM在山区的精度最高。具体表现在：1）3套产品在降水较多的夏秋季均表现较好,相对于TRMM与CMORPH,GPM与观测数据的相关系数最高（R≥0.6）,相对误差最小（PB≈10%）;2）在整个天山山区,GPM相对于其他两套产品表现出较低的误差范围（-55%~55%）;3）GPM在不同的高程带内,均表现出同观测站点较低的误差与较高的相关系数;4）3套降水产品均表现出对探测弱降水事件较高的准确性（POD≈0.58）和较低的错误率（FAR≈0.63）,但综合分析4种指数,GPM表现最佳,能够以较准确的精度和较低的误差估测降水系统。     

地球系统模式CESM模拟的ENSO变率与中国东部降水格局

根据地球系统模式（CESM）的千年控制模拟试验结果,以Niño3.4区的逐月海表温度变化为指标,辨识了212次El Niño事件、226次La Niña事件;分析了El Niño和La Niña事件发生当年及次年中国东部5-9月降水异常的空间格局;探讨了ENSO与华北、江淮、江南和华南4个区域旱涝的关系。结果表明：El Niño事件发生的当年5-9月,华北和华南地区降水减少2%~10%,长江中下游地区降水略有增加（0~2%）;次年,江南地区转为降水增加（2%~10%）,华北北部降水继续减少。在La Niña事件发生的当年,华北地区降水偏多（增加2%~10%）;次年,江淮地区降水显著减少（2%~5%）。ENSO增强会导致降水变幅加大。在El Niño衰减并向La Niña快速发展的年份,江南地区出现洪涝灾害的概率较其他年份高1倍以上。这些认识为深入揭示气候系统内部年际变率对中国东部降水格局变化与区域旱涝的影响作用、理解2016年长江中下游发生重大洪涝灾害提供了异常天气气候背景依据。     

基于平稳与非平稳GEV模型的鄱阳湖流域极值降水模拟

论文基于鄱阳湖流域降水数据,采用平稳和非平稳GEV模型进行极值降水的模拟和分析。检测各站年最大1 d降水量序列（AMS1）的非平稳特征,将时间作为位置参数的协变量进行非平稳AMS1序列的GEV模拟。结果表明：1）鄱阳湖流域AMS1序列的形状参数基本均大于0,服从Fréchet分布;位置和尺度参数的空间分布较一致,形状参数则有差异。2）在较高重现期下由轮廓似然方法估计的置信区间比Delta方法更准确;重现水平的轮廓似然函数曲线在较高重现期之下呈较显著不对称性。3）不同重现期下的鄱阳湖流域极值降水等值线图的空间分布特征,与位置和尺度参数的分布图更为接近,与形状参数的差别则较大。4）基于非平稳GEV模型得到赣县站随时间变化的极值降水设计值,其在1951年的100 a一遇设计值到2010年下降为接近50 a一遇,预示着未来发生极值降水和洪灾的风险加大。     

Fe-Mn-sepiolite as an effective heterogeneous Fenton-like catalyst for the decolorization of reactive brilliant blue

A study of the decolorization of reactive brilliant blue in an aqueous solution using Fe-Mn-sepiolite as a heterogeneous Fenton-like catalyst has been performed. The Fourier transform infrared (FTIR) spectra of the catalyst showed bending vibrations of the Fe-O. The X-ray diffraction (XRD) patterns of the catalyst showed characteristic diffraction peaks of α-Fe₂O₃, γ-Fe₂O₃ and MnO. A four factor central composite design (CCD) coupled with response surface methodology (RSM) was applied to evaluate and optimize the important variables (catalyst addition, hydrogen peroxide dosage, initial pH value and initial dye concentration). When the reaction conditions were catalyst dosage= 0.4 g, [H₂O₂]= 0.3 mL, pH= 2.5, [reactive brilliant blue]_o = 50 mg·L⁻¹, and volume of solution= 500 mL at room temperature, the decolorization efficiency of reactive brilliant blue was 91.98% within 60 min. Moreover, the Fe-Mn-sepiolite catalyst had good stability for the degradation of reactive brilliant blue even after six cycles. Leaching of iron ions (<0.4 mg·L⁻¹) was observed. The decoloring process was reactive brilliant blue specific via a redox reaction. The benzene ring and naphthalene ring were first oxidized to open ring; these were then oxidized to the alcohol and carboxylic acid. The reactive brilliant blue was decomposed mainly by the attack of ·OH radicals including surface-bound ·OH radicals generated on the catalyst surface.     

基于TRMM订正数据的横断山区降水时空分布特征

鉴于高时空变异地区降水观测的需求,论文提出了基于ISODATA动态聚类法和最大似然法分区逐月回归的TRMM数据订正方法,并以横断山区为例,利用地基台站降水数据对1998-2012 年的TRMM 3B43 V7 数据进行了实验研究,并探讨了过去15 a 横断山区的降水时空分布特征及变化趋势。结果表明,TRMM 3B43 V7 数据在横断山区的总体精度较高,单站精度较低。订正后的TRMM 3B43 数据,与实测值偏差大为减少,降水相对偏差大于10%的站点由原始数据的16 个(42.1%)减少为7 个(18.4%),有81.6%的站点年降水量相对偏差小于10%,且相对偏差大于等于20%的站点仅3 个,能够基本满足横断山区降水时空分布特征研究的精度需要,有效地弥补了有限站点观测的不足。研究区内年降水量从东南向西北递减,与东亚季风在该区域的走向一致;1998-2012 年横断山区的降水量主要呈减少趋势,减少地区主要分布在南部以及中西部地区。夏季降水减少趋势最为突出,秋季次之,冬春变化趋势不明显。横断山区大部分区域的降水量与东亚夏季风指数正相关,与东亚冬季风指数负相关;最近15 a,研究区东亚季风指数持续变小,恰好与研究结果中的降水减少趋势一致。