Strong, low frequency (decadal) environmental fluctuations during the 20th century in the North Pacific Ocean, on the Washington coast, and in Puget Sound

At decadal period (10-20 years), dynamic linkage was evident between atmospheric low pressure systems over the North Pacific Ocean and circulation in a Pacific Northwest fjord (Puget Sound). As the Aleutian low pressure center shifts, storms arriving from the North Pacific Ocean deposit varying amounts of precipitation in the mountains draining into the estuarine system; in turn, the fluctuating addition of fresh water changes the density distribution near the fjord basin entrance sill, thereby constraining the fjord's vertical velocity structure. This linkage was examined using time series of 21 environmental parameters from 1899 to 1987. Covariation in the time series was evident because of the strong decadal cycles compared with long-term averages, interannual variability, and seasonal cycles.

Inferences from tree rings on low frequency variations in runoff in the interior western United States

EXTRACT (SEE PDF FOR FULL ABSTRACT): Low frequency variations in runoff, AD 1700-1964, in the interior western United States are inferred from smoothed tree-ring series averaged over north, central, and south regions. ... Relative locations of peaks and troughs in streamflow, precipitation, temperature, and tree-ring series suggest that annual precipitation and warm season evapotranspiration variations may both be important to low frequency fluctuations in tree growth and in streamflow.

El Niño-Southern Oscillation (ENSO) phenomena and forest fires in the southwestern United States

Fire statistics (area burned) and fire-scar chronologies from tree rings show reduced fire activity during El Niño-Southern Oscillation (ENSO) in forests of Arizona and New Mexico. This relationship probably stems from increased fuel moisture after a wet winter and spring, but also could involve climatic controls on lightning activity at the onset of the monsoon season.

Centennial oscillation of the climatic crescendo during the last glacial maximum: evidence from Lake Estancia, central New Mexico

Sediments deposited in late Pleistocene Lake Estancia, central New Mexico, contain a paleoclimatic record that includes the last glacial maximum and deglacial episode. Stratigraphic reconstruction of an interval representing the highstand of the lake that occurred during the last glacial maximum reveals ~2000-, ~600-, and ~200-year oscillations in lake level and climate. Shifting position of the polar jetstream in response to expansion and contraction of the North American ice sheet may be partly responsible for the millenial-scale changes in Lake Estancia but probably does not explain the centennial-scale oscillations.

South American streamflow and the extreme phases of the Southern Oscillation

This study investigates the extent of the affect [sic] of the El Niño/Southern Oscillation on South American streamflow. The response of South American precipitation and temperature to the extreme phases of ENSO (El Niño and La Niña events) is well documented; but the response of South American hydrology has been barely studied. Such paucity of research contrasts sharply with that available on the response of North American streamflow to ENSO events.

根茎克隆植物羊草分株种群对去叶干扰的生长对策

克隆植物具有多种不同于非克隆植物的生长和繁殖策略。本研究首先综述了这些生长与繁殖策略之中，与我们的实验研究相关的尤其是对于去叶干扰适应策略的四个方面，包括克隆整合、克隆分株大小与密度之权衡( tradeoff)过程、碳水化合物贮备与利用、营养繁殖和芽种群(bud population)调节等。预测克隆植物选择什么样的对策以及某种对策发生作用的条件及程度如何，对克隆植物生态学研究者来说，将是富有挑战意味的课题。 羊草(Leymus chinensis (Trin,) Tzvel.)是禾本科的一种多年生根茎型克隆植物，常常处于由放牧或刈割造成的去叶干扰( defoliation)的胁迫下。在我们的第一个实验（2002年）中，考察了去叶干扰和根茎切割( rhizome severing)是否影响根茎本身和分株地上部分的生长、以及营养繁殖芽的数量特征。同时我们检验如下的假设：直接受到去叶干扰的分株除了会受益于可能的补偿作用之外，还会受益于克隆整合作用，即与之保持根茎联系的未受去叶处理的分株将转移碳水化合物或养分给受去叶干扰的分株，使之得以尽快恢复光合组织。实验结果显示：单次去叶干扰影响根茎生长和芽的产生，而对地上部分的生长影响甚微。只有重度去叶干扰才显著影响营养繁殖芽的产生，而轻度去叶干扰作用不明显。所以，当去叶强度不大时，补偿作用机制将弥补植物由于去叶干扰而受到的损失。我们的实验并未检测到克隆整合的发生，可能的原因是本实验持续的时间不足够长或者是由于根茎中的碳水化合物贮备在去叶干扰发生后发挥了作用，缓解了去叶干扰对羊草分株生长及芽生产的所造成的冲击。 在第二个实验（200 3年）中，为了考查相继数次的去叶干扰是否能够启动羊草分株间的克隆整合，以及启动克隆整合所需达到的去叶干扰的频次，我们将实验样方设计为两部分：核心区( Core section)和外围区(Periphery section)。不同频次的去叶处理（0去叶，作为对照; 1次去叶;3次去叶;5次去叶）仅施加于实验样方的核心区。结果表明，经历3次和5次去叶处理的样方外围区的生物量及水溶性碳水化合物( wsc)含量均明显少于经历1次去叶处理及0去叶处理的样方外围区，这意味着克隆整合在3次去叶和5次去叶两种处理中发生了，而在其它两种处理中没有发生。此外，分株的大小一数目之权衡可能在基株(genet)水平上发生，因此，一个克隆植物基株，当部分分株受到去叶干扰后，将增加其分株数目，但优先增加未受到去叶干扰部分的分株数目。我们将羊草的这种行为视为克隆基株试图逃避干扰的“逃逸行为”( escaping behavior)。 同时在实验中，我们监测了实验样方核心区分株的wsc浓度，目的是查明羊草枝条与根茎中wsc浓度随时间的变化格局及其对去叶干扰的响应，意在发现羊草枝条地上、地下部分和根茎中wsc浓度的时间变化之间的联系。在生长旺季，对照处理（即O去叶处理）的wsc浓度显著降低，这是由于植物在此时期的高生长速率和高呼吸速率所致;相比之下，其它经历去叶干扰的三个处理中羊草wsc浓度降低不如对照处理那么明显和迅速，甚至在高频次去叶处理中还有所上升，其原因大概是由于去叶而使叶面积减小，引起枝条的总呼吸下降所致。羊草枝条中最终的wsc浓度没有受到单次去叶处理的显著影响，却很可观地受到相继数次去叶干扰（3次和5次去叶处理）的影响。去叶干扰可能加速了碳水化合物在气温降低时自地上向地下的转移。枝条的地下部分wsc浓度比地上部分更稳定。在地上部分受到去叶干扰后，根茎中的wsc必然向上输出到地上枝条，而强烈的生长会消耗wsc，但可能的克隆整合（通常在相对频繁的去叶干扰条件下发生）将在一定程度上缓解这种wsc消耗。 在此实验中，我们还监测了羊草平均每分株所拥有的芽的数目，包括每分株分蘖节芽（tiller bud）数目和根茎芽(thizomatous bud)数目。从平均每分株芽数目的时间动态来看，各种去叶处理之间的差异程度不大，这主要是羊草在受到去叶干扰后补偿作用的贡献。与对照处理相比，受不同频次去叶干扰的三个处理的根茎芽具有相对于分蘖节的更强的增长优势。去叶干扰对根茎芽生长的促进作用大于对分蘖节芽的促进作用。我们认为这种反应是羊草克隆基株的一种逃避干扰的适应性努力，可视为一种“逃逸行为”，也可看作克隆植物觅养行为(foraging behavior)的一种特殊形式。芽的增长在中等频度的去叶干扰条件下最强，似乎同样符合中度干扰理论。有趣的是，特定频度的去叶干扰可能会造成芽种群中两大类型芽之间比例（根茎芽／分蘖节芽）的振荡现象（Oscillation）。 最后展望了对于羊草今后应继续开展的工作主要集中在两大方面：一是有性繁殖与无性繁殖之间在不同生境或不同干扰条件下的权衡关系;二是处于不同斑块对比度( patch contrast)的生境中的羊草克隆分株之问的生理整合，及其强度与斑块对比度的定量关系。

Length frequency and growth studies on Cynoglossus macrolepidotus (Bleeker) off Bombay coast

Specimens randomly collected from Sassoon Docks, Bombay, India, at monthly intervals during 1979 to 1981 were considered for age/growth studies. Cynoglossus macrolepidotus, the fish, attained a length of 202 mm at 1 year, 250 mm at 1 1/2 year and 272 mm at 21 months respectively; the maximum length of the fish could be 353 mm and the life span could be 7 years. The scale ring studies showed presence of only 0 to 3+ rings. Majority of the fishes were of 1 and 1+ year class.